Archean geology of a part of the northern Gallatin Range, southwest Montana
by Karen Anne May
A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in
Earth Sciences
Montana State University
© Copyright by Karen Anne May (1985)
Abstract:
The northern Gallatin Range in southwest Montana is predominantly composed of regionally
metamorphosed Archean quartzofeldspathic gneisses with minor amounts of metabasites. This study
characterizes the petrography, petrology, and structure of Archean rocks exposed in a part of the
northern Gallatin Range to determine the Archean tectonic evolution of this part of southwest Montana.
Metamorphism in the study area ranges from epidote-amphibolite to transitional granu-Iite facies.
These rocks are believed to have initially experienced a transitional granulite facies metamorphic event
(M1) followed by epidote-amphibolite facies conditions (M2). Retrograde assemblages in the study
area rocks may be indicative of a greenschist thermal event (M3?). A dominant N45E structural grain is
expressed by foliation strikes and fold hinge line trends. Polyphase deformation is evident based on the
identification of two fold generations. Isoclinal folds were produced during an earliest (M1) event.
Coaxial open folds were subsequently produced during M2. The tectonic setting for study area rocks is
best represented by an ensialic basin depositional environment that was subsequently deformed via
A-type subduction processes. ARCHEAN
geology of a p a r t of the northern
GALLATIN RANGE, SOUTHWEST MONTANA
by
K a re n Anne May
A t h e s i s su b m itte d in p a r t i a l f u l f i l l m e n t
o f th e re q u ire m e n ts f o r th e d egree
of
M aster o f S cien ce
in
E a r th S c ien c e s
MONTANA STATE UNIVERSITY
Bozeman, M ontana
D e cem ber, 1985
MAIN LIS.
N3?g
n w
(Lop. 3U
ii
APPROVAL
o f a t h e s i s s u b m i t t e d by
K a re n Anne May
T h i s t h e s i s h a s b e e n r e a d by e a c h member o f t h e t h e s i s c o m m i t t e e
and h as b e e n fo u n d t o be s a t i s f a c t o r y r e g a r d i n g c o n t e n t , E n g l is h
u s a g e , f o r m a t , c i t a t i o n s , b i b l i o g r a p h i c s t y l e , and c o n s i s t e n c y , and i s
read y f o r s u b m is s io n to th e C o lle g e o f G rad u ate S tu d ie s .
D a te
C h a i r p e r s o n , G r a d u a t e Com m ittee
A pproved f o r t h e M a jo r D e p a rtm e n t
Approved f o r t h e C o l l e g e o f G r a d u a te S t u d i e s
1 /% ^
D a te
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G r a d u a t e Dean
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STATEMENT OF PERMISSION TO USE
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th e
r e q u i r e m e n t s f o r a m a s t e r 's d e g r e e a t M o n ta n a S t a t e U n i v e r s i t y ,
a g r e e t h a t t h e L i b r a r y s h a l l m ake i t
r u le s of th e L ib ra ry .
I
a v a ila b le to b o rro w ers under
B r i e f q u o t a t i o n s f ro m t h i s t h e s i s a r e a l l o w a b l e
w ith o u t s p e c ia l p erm issio n ,
p r o v i d e d t h a t a c c u r a t e a c k n o w le d g m e n t o f '
s o u r c e i s m ade.
P e r m i s s i o n f o r e x t e n s i v e q u o t a t i o n fro m o r r e p r o d u c t i o n o f t h i s
t h e s i s may b e g r a n t e d b y my m a j o r p r o f e s s o r , o r i n h i s a b s e n c e , b y t h e
D i r e c t o r o f L i b r a r i e s w hen, i n t h e o p i n i o n o f e i t h e r , t h e p r o p o s e d u s e
of th e m a te ria l is
f o r s c h o la rly purposes.
m a te ria l in t h is th e s is
f o r f i n a n c i a l g a in s h a l l n o t be a llo w e d w ith ­
o u t my w r i t t e n p e r m i s s i o n .
S ig n a tu re
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Q p n m ^
Any c o p y in g o r u s e o f t h e
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To my p a r e n t s , f o r t w e n t y - n i n e y e a r s o f p a t i e n c e an d s u p p o r t .
V
ACKNOWLEDGMENTS
I am i n d e b t e d t o s e v e r a l p e o p l e f o r s u p p o r t i n g me d u r i n g t h i s
stu d y .
T hanks a r e e x t e n d e d t o Dr. D a v id Mogk f o r h i s g u i d a n c e and f o r
s h a r i n g h i s k n o w l e d g e o f A rc h e a n t e c t o n i c s
i n s o u t h w e s t M ontana,
and
t o D r. L a g e s o n , D r. J o h n M o n ta g n e , and D r. C l i f f M o n ta g n e f o r t h e i r
i n s i g h t and a s s i s t a n c e . The l a t e D r. D o n ald . S m ith p r o v i d e d v a l u a b l e
e n c o u r a g e m e n t a t a n e a r l y s t a g e o f my g r a d u a t e c a r e e r .
a s sista n c e
w as g r a t e f u l l y
re c e iv e d
from
th e
C o lleg e
F in a n c ia l
o f G ra d u a te
S t u d i e s t h r o u g h t h e R e s e a r c h C r e a t i v i t y P ro g ra m and t h r o u g h a G r a d u a te
T each in g A s s i s t a n t s h i p aw arded b y t h e D e p a r tm e n t o f E a r t h S c i e n c e s .
A p p r e c i a t i o n i s e x t e n d e d t o M r. Norm B u h l o f t h e G a l l a t i n N a t i o n a l
F o r e s t f o r v e h i c l e a c c e s s a lo n g th e S ourdough C reek F o r e s t S e r v ic e
R o a d , a n d t o M r s . H e l e n C l a r k , Mr. M y l e s H u p k a , a n d D r . J o h n M o n ta g n e
f o r p ro v id in g a c c e ss to th e stu d y a re a th ro u g h t h e i r p r iv a t e p ro p erty .
C a r o l C r a ig l o w c o n t r i b u t e d h e r a r t i s t i c
t a l e n t and S h a ro n D u s e n b e r r y -
Tank p r o v i d e d t h e f i n a l t o u c h e s on t h e m a n u s c r i p t .
S p e c ia l th an k s a r e
e x t e n d e d t o t h e many f r i e n d s who h a v e p r o v i d e d m o r a l s u p p o r t and f i e l d
a ssista n c e .
EBBATA
The f o l l o w i n g c o r r e c t i o n s s h o u l d h e n o t e d :
The l o c a t i o n a b b r e v i a t i o n s S - 1 3 bind S - 1 4 f o u n d on t h e f o l l o w i n g p a g e s
s h o u l d i n s t e a d r e a d 8 - 1 2 a n d S - 13, r e s p e c t i v e l y :
page
page
page
page
48
51
55
84
( t e x t o n l y - f i g u r e c a p t i o n on t h i s page i s c o r r e c t ) ,
T h in s e c t i o n l a b e l S -1 3 on t a b l e
rJ 9 page 91 s h o u ld i n s t e a d r e a d S-43
vi
TABLE OF CONTENTS
Page
1.
LIST OF TABLES.......................................................................................................
v ii
2.
LIST OF. FIGURES..........................................
j.x
3.
ABSTRACT......................................................................................................................
xi
4.
INTRODUCTION...............................
I
I
5.
REGIONAL GEOLOGIC SETTING.............................................................................
7
6.
PETROLOGY..................................
9.
Q u a r t z o f e l d s p a t h i c G n e i s s e s ............................................................
F i e l d O c c u r r e n c e .....................................................
M i n e r a l o g y ............................................................................................
R e t r o g r a d e A s s e m b l a g e s .......................................................
T e x t u r e s ................................................................................................
D e f o r m a t i o n a l and R e c r y s t a l l i z a t i o n E f f e c t s ............
P r o t o l i t h .......................................................
M i g m a t i t e s .............................................................
A m p h i b o l i t e F a c i e s M e t a b a s i t e s ...........................................
F i e l d O c c u r r e n c e ............................................
M i n e r a l o g y ............................................................................................
T e x t u r e s ................................................................................................
U n iq u e O c c u r r e n c e s ........................
T r a n s i t i o n a l G r a n u l i t e F a c i e s ........................................................
M i n e r a l o g y ............................................................................................
T e x t u r e s .............................................
P r o t o l i t h ............................. ........................................ .....................
O ' 4s- - >
F o re w o rd an d S t a t e m e n t o f P u r p o s e .................................................
M ethods o f I n v e s t i g a t i o n
L o c a t i o n and A c c e s s ..........
P r e v i o u s S t u d i e s .................
9
9
10
13
13
14
15
19
23
23
23
26
27
31
31
32
36
7.
MYLONITES...........................................
38
8.
METAMORPHISM............................................................................................................
44
9.
DEFORMATION...........................................................................................
47
CORRELATION OF METAMORPHISMAND DEFORMATION.....................................
57
10 .
v ii
TABLE OF CONTENTS— C o n tin u e d
Page
11.
TECTONIC MODEL.................................................................
61
A ndean-T ype S u b d u c t i o n ........................................................................
The Q u e s t i o n o f A c c r e t i o n .................................................................
A-Type S u b d u c t i o n .................................................................................
63
65
67
12 .
SUMMARY AND CONCLUSIONS..................................................................................
71
13.
REFERENCES CITED...................................................................................................
73
14.
APPENDICES.................................................................................................................
82
A p p e n d ix A
L o c a t i o n s o f M a jo r O u t c r o p s t h a t w e re
S t u d i e d i n D e t a i l . ...........................................
A p p e n d ix B
M in e ra l C o n te n ts o f Q u a r tz o f e ld s p a th ic
G n e i s s e s ...........................................
A p p e n d ix C
M i n e r a l C o n t e n t s o f A m p h i b o l i t e F a c i e s .........................
A p p e n d ix D
M i n e r a l C o n t e n t s o f T r a n s i t i o n a l G r a n u l i t e s .............
83
85
88
90
v iii
LIST OF TABLES
T ab le
Page
1.
M in e ra l a sse m b la g e s o f q u a r t z o f e l d s p a t h i c g n e is s e s '
a n d q u a r t z i t e s ................................................................................................
2.
A m p h i b o l i t e f a c i e s m e t a b a s i t e a s s e m b l a g e s .....................................
24
3.
T r a n s itio n a l g r a n u l i te f a c ie s m e ta b a site a s s e m b la g e s .....
32
4.
I n t e r p r e t e d g e o c h r o n o l o g y o f m e t a m o r p h ic and
d e fo rm a tio n a l e v e n ts a f f e c ti n g basem ent l i t h o l o g i e s in
t h e n o r t h e r n G a l l a t i n R a n g e . . . . ............ ...........................................
60
5.
M i n e r a l c o n t e n t s o f q u a r t z o f e l d s p a t h i c g n e i s s e s ......................
86
6.
M i n e r a l c o n t e n t s o f a m p h i b o l i t e f a c i e s ...............................
89
7.
M i n e r a l c o n t e n t s o f t r a n s i t i o n a l g r a n u l i t e s .....................
91
ix
LIST OF FIGURES
F ig u re
Page
1.
Wyoming A r c h e a n P r o v i n c e ........................................... .................... i
2.
I n d e x map o f t h e n o r t h e r n Wyoming A rc h e a n P r o v i n c e ...............
3
3.
G e n e r a l i z e d g e o l o g i c and i n d e x map f o r s t u d y a r e a .................
5
4.
Q u a r t z o f e l d s p a t h i c g n e i s s c o m p o s i t i o n s .....................
12
5.
M o b i l i z e d le u c o s o m e w i t h i n m a f i c g n e i s s
(m esosom e)................
20
6.
N o n - d i r e c t i o n a l le u c o s o m e w i t h i n m et ah a s i t e u n i t ....................
21
7.
ACF d i a g r a m s i l l u s t r a t i n g d o m in a n t s t a b l e and
r e t r o g r a d e a ssem b lag es i n s tu d y a r e a a m p h ib o lite
f a c i e s m e t a b a s i t e s ..........................................................................
25
Pod ( c r o s s - h a c h u r e d p a t t e r n ) i n s h a r p c o n t a c t w i t h
q u a r t z o f e l d s p a t h i c g n e i s s e s ( q f g n ) .................................
28
9.
C a t a c l a s t i c p o d s i n h i g h l y w e a t h e r e d s h e a r z o n e . . . . . ..........
29
10 .
L e n s - s h a p e d a c t i n o l i t i t e p o d ....................................................................
30
11.
L e n s - s h a p e d t r a n s i t i o n a l g r a n u l i t e m et a b a s i t e ...........................
33
12.
ACF d ia g r a m f o r c o r o n a t e x t u r e m e t a b a s i t e ....................................
35
13.
U l t r a m y l o n i t e ........................................................................................
39
14 .
P s e u d o t a c h y l y t e t e x t u r e ..........................................................................
42
15 .
T e m p e r a t u r e - p r e s s u r e d i a g r a m f o r m etam orphism o f t h e
s t u d y a r e a ...............................................................................................................
45
16.
G e n e r a l i z e d s t r u c t u r e map f o r s t u d y a r e a .......................................
48
17 .
S te re o n e ts i l l u s t r a t i n g th e g e n e ra l s t r i k e of
f o l i a t i o n fro m m a j o r o u t c r o p s w i t h i n t h e s t u d y
a r e a .............................................................................................................................
49
B i o t i t e s t r e a k and a m p h ib o le m i n e r a l l i n e a t i o n
s t e r e o n e t s ...............................................................................................................
50
I s o c l i n a l and o p e n f o l d h i n g e l i n e s t e r e o n e t s ...........................
51
8.
18.
19.
. . . .
2
X
LIST OF FIGURES— C o n tin u e d
20.
I s o c l i n a l (F l) i n t r a f o l i a l f o ld i n g o f l e u c o c r a t i c u n i t
(L) w i t h i n q u a r t z o f e l d s p a t h i c g n e i s s ( q f g n ) .............................
52
D i s h a r m o n i c a l l y f o l d e d ( F l ) q u a r t z o f e l d s p a t h i c and
a m p h i b o l i t e g n e i s s e s ......................................................................................
53
22.
Open t o b r o a d f l e x u r a l - f l o w f o l d s
( F 2 ) ............ ...............................
54
23.
S u p e r p o s e d f o l d s o f dome and b a s i n f o r m .........................................
55
24.
S u g g e s te d s t a g e s i n t h e A r c h e a n t e c t o n i c e v o l u t i o n o f
s o u t h w e s t M ontana ( e x c l u d i n g t h e B e a r t o o t h Range)
in v o lv in g A -ty p e ( c o n t i n e n t a l) s u b d u c tio n
68
21.
xi
ABSTRACT
The n o r t h e r n G a l l a t i n Range i n s o u t h w e s t M ontana i s p r e d o m i n a n t l y
com posed o f r e g i o n a l l y m etam o rp h o sed A rchean q u a r t z o f e l d s p a t h i c
g n e i s s e s w i t h m i n o r a m o u n ts o f m e t a b a s i t e s .
T h is s tu d y c h a r a c t e r i z e s
t h e p e t r o g r a p h y , p e t r o l o g y , and s t r u c t u r e o f A r c h e a n r o c k s e x p o sed i n
a p a r t o f t h e n o r t h e r n G a l l a t i n Range to d e te r m i n e t h e A rch ean t e c ­
t o n i c e v o l u t i o n o f t h i s p a r t o f s o u t h w e s t M ontana.
M eta m o rp h ism i n
t h e s t u d y a r e a r a n g e s fro m e p i d o t e —a m p h i b o l i t e t o t r a n s i t i o n a l g r a n u —
I i t e fac ies.
These ro c k s a r e b e l i e v e d t o have i n i t i a l l y e x p e rie n c e d a
t r a n s i t i o n a l g r a n u l i t e f a c i e s m e t a m o r p h i c e v e n t (M l) f o l l o w e d b y
e p i d o t e —a m p h i b o l i t e f a c i e s c o n d i t i o n s (M2). R e t r o g r a d e a s s e m b l a g e s i n
t h e s t u d y a r e a r o c k s may b e i n d i c a t i v e o f a g r e e n s c h i s t t h e r m a l e v e n t
(M 3?). A d o m i n a n t N45E s t r u c t u r a l g r a i n i s e x p r e s s e d b y f o l i a t i o n
s t r i k e s and f o l d h i n g e l i n e t r e n d s .
P o ly p h ase d e fo r m a tio n i s e v id e n t
b a s e d on t h e i d e n t i f i c a t i o n o f tw o f o l d g e n e r a t i o n s .
I s o c lin a l fo ld s
w e r e p r o d u c e d d u r i n g an e a r l i e s t (Ml) e v e n t .
C o a x i a l op e n f o l d s w e r e
s u b s e q u e n t l y p r o d u c e d d u r i n g M2.
The t e c t o n i c s e t t i n g f o r s t u d y a r e a
r o c k s i s b e s t r e p r e s e n t e d b y an e n s i a l i c b a s i n d e p o s i t i o n a l e n v i r o n ­
m ent t h a t w as s u b s e q u e n t l y d e f o r m e d v i a A—t y p e s u b d u c t i o n p r o c e s s e s .
I
INTRODUCTION
F o re w o rd and S t a t e m e n t o f P u r p o s e
The n o r t h e r n G a l l a t i n
Range i n s o u t h w e s t M o n ta n a l i e s i n t h e
n o r t h w e s t e r n p a r t o f t h e W yom ing A r c h e a n P r o v i n c e ( F i g u r e I ) a n d i s
p re d o m in a n tly
com posed
of
re g io n a lly
m e ta m o rp h o se d
A rchean
q u a rtz o f e ld s p a th ic g n e is s e s w ith m in o r a m o u n ts o f m e t a b a s i t e s .
m e t a m o r p h ic g r a d e o f t h e s e
tra n sitio n a l
te c to n ic
g ra n u lite
s e ttin g
rocks
ranges
fac ies.
fro m e p i d o t e —a m p h i b o l i t e t o
The n a t u r e
f o r A rchean ro c k s
of
p ro to lith s
and
a
i n s o u t h w e s t M o n ta n a i s c u r r e n t l y
s p e c u l a t i v e and i n c o m p l e t e l y u n d e r s t o o d .
s ta te
T he
As a r e s u l t , o u r p r e s e n t
o f k n o w led g e o f A rchean e v o lu tio n , o f c o n t i n e n t a l c r u s t in t h i s
area is lim ite d .
The s t u d y a r e a i s
lo c a te d near th e tr a n s itio n
fro m
p r e d o m i n a n t l y i g n e o u s and m e t a - i g n e o u s r o c k s i n t h e B e a r t o o t h Range t o
t h e e a s t an d a p r e d o m i n a n t l y m e t a s u p r a c r u s t a l t e r r a n e i n t h e r a n g e s t o
th e w est
(F ig u re
2,
Mogk e t a l ,
a d d itio n a l p e tro g ra p h ic ,
in
p e tro lo g ic ,
re v ie w ).
T h is
s tu d y p ro v id e s
an d s t r u c t u r a l d e t a i l f o r a p a r t
of th e A rchean ro c k s in t h i s c r i t i c a l t r a n s i t i o n a r e a .
M y lo n ite s,
m ig m a t i t e s , and t r a n s i t i o n a l g r a n u l i t e s p r e s e n t in th e s tu d y a r e a
p r o v i d e d e t a i l s v i t a l t o a n a n a l y s i s o f t h e A rc h e a n t e c t o n i c e v o l u t i o n
o f s o u t h w e s t M ontana.
The o b j e c t i v e s o f t h i s r e s e a r c h a r e t h r e e f o l d :
I) t o d e s c r i b e t h e
l i t h o l o g i e s and s t r u c t u r e s o f t h e A r c h e a n b a s e m e n t r o c k s p r e s e n t i n
th e stu d y a re a ,
2) t o c h a r a c t e r i z e t h e i r p e t r o g e n e s i s and s u b s e q u e n t
A p p ro x im a te W yom ing
Province b o u n d a r y
T obacco Bool Mins.
M a d iso n B a n g e
MONTANA
• Cody
Big Horn Mins.
Beoiioolh Mlns
Telon B a nge
Wind Biver B a n g e
• Jockion
M ounloins
IDAHO
M edicine Bow B a n g e
COLORADO
Sierra M a d r e Bonge
F ig u re I .
Wyoming A rc h e a n P r o v i n c e ( a f t e r C o n d i e , 1975)
'
Nor t h S n o w y Bl o c k
Mo b i l e Bel t
|-r) ' y n c u u s
ana
Metaigneous Rocks
T o b a c c o Root Mtns.
Ruby R a n g e
■
Madi s on Ra n g e
Gallatin Range
M etasupracrustal
I Rocks
North Snowy Block
B e a r t o o t h Mount ai ns
MONTANA
IDAHO
MONTANA
Big Horn Mt ns. V . * i
Te t o n Ra n g e
Wind River Range
F ig u re 2.
I n d e x map o f t h e n o r t h e r n p o r t i o n o f t h e A rc h e a n Wyoming P r o v i n c e . The N o rth Snowy
B lo c k m o b il e b e l t s e r v e s a s a l o c a l b o u n d a r y , s e p a r a t i n g p r e d o m i n a n t l y ig n e o u s and
m e t a - i g n e o u s r o c k s t o t h e e a s t from p r e d o m i n a n t l y m e t a s u p r a c r u s t a l r o c k s t o t h e w est
(fro m Mogk, e t a l , i n r e v i e w ) .
4
sty le
of
d e fo rm a tio n ,
and
3) t o
p lac e
th em
in
th e
c o n te x t
of
a
r e g i o n a l A r c h e a n s e t t i n g and d e v e l o p a t e c t o n i c i n t e r p r e t a t i o n .
M ethods o f I n v e s t i g a t i o n
The sum m er f i e l d
rock
sp e c im e n s,
re la tio n sh ip s.
lith o lo g ic
s e a s o n s o f 1982 and 1983 w e r e s p e n t c o l l e c t i n g
s tru c tu ra l
d a ta ,
The s p o r a d i c n a t u r e
m ap p in g
of
th e
stu d y
and
o b se rv a tio n s
of ex p o su res
area.
About
of
d id n o t w a rra n t
100 o u t c r o p s
o b s e rv e d , th o u g h m ost w ere to o s m a ll o r i n s u f f i c i e n t l y
y ie ld v a lu a b le d a ta .
w ere
stu d ie d
re p re se n ta tiv e
stu d y
area.
in
w ere
exposed to
F o u r u n i q u e o u t c r o p s s u b s t a n t i a l e n ough i n s i z e
d e ta il
as
of lith o lo g ie s
T hese
fie ld
o u tc ro p s
s e p a ra te
d o m a in a l
and s t r u c t u r e s
are
h ig h lig h te d
u n its
observed
and
are
th ro u g h o u t th e
th ro u g h o u t
( l o c a t i o n s o f t h e s e m a j o r o u t c r o p s a p p e a r i n A p p e n d ix A).
th e
te x t
One h u n d r e d
and f o r t y - s e v e n r o c k s w e r e c o l l e c t e d and 57 t h i n s e c t i o n s r e p r e s e n t a ­
tiv e
o f th e m ajo r l i t h o l o g i c
u n its
and u n iq u e l i t h i o l o g i e s w ere p r e ­
p a re d f o r d e t a i l e d p e tr o g r a p h ic stu d y .
i d e n t i f y t h e m i n e r a l o g y o f one r o c k .
X - r a y d i f f r a c t i o n was u s e d t o
S t r u c t u r a l d a t a w e r e p l o t t e d on
s te r e o n e ts to a id in th e a n a ly s is of s t r u c t u r a l e le m en ts.
L o c a t i o n and A c c e s s
The s t u d y a r e a l i e s
m i l e s s o u t h o f Bozem an,
in th e n o rth e rn G a lla tin
M ontana and i s c o v e r e d by t h e U.S.G.S. Bozeman
1 5 -m in u te q u a d r a n g le ( F ig u r e 3).
th e w e st.
Range a b o u t s i x
I t i s b o u n d e d b y H y a l i t e C r e e k on
S ourdough C reek to th e e a s t ,
th e G a l l a t i n V a lle y to th e
n o r t h , t h e r e s t o f t h e G a l l a t i n Range t o t h e s o u t h , and e n c o m p a s s e s an
5
F ig u re 3.
G e n e r a l i z e d g e o l o g i c a n d i n d e x map f o r s t u d y a r e a ( a f t e r
R o ss, e t a l , 1955). L i t h o l o g i e s a r e :
P recam b rian g n e iss
and s c h i s t (pCgs), P a l e o z o i c and M e so z o ic s e d i m e n t a r y u n i t s
u n d i f f e r e n t i a t e d (P z/M ), C r e t a c e o u s d i o r i t e and g a b b ro
(K dg), T e r t i a r y w a t e r - l a i d v o l c a n i c m a t e r i a l (T kI),
T e r t i a r y v o l c a n i c s (Tv), a n d Q u a t e r n a r y a l l u v i a l d e p o s i t s
(Q ) . Heavy o u t l i n e i n d i c a t e s s t u d y a r e a .
6
a re a o f about seven sq u are m ile s .
p r e s e n c e o f A rc h e a n r o c k s ,
A ccess
to
th e
s tu d y
The a r e a w as c h o s e n b e c a u s e o f t h e
p r o x i m i t y , t o Bozeman,
area
w as
g a in e d
by
and e a s e o f a c c e s s .
p e rm issio n
of
p riv a te
l a n d o w n e r s an d t h r o u g h t h e u s e o f F o r e s t S e r v i c e and p u b l i c r o a d s .
P re v io u s S tu d ie s
A l i m i t e d a m o u n t o f i n f o r m a t i o n i s a v a i l a b l e on A r c h e a n r o c k s
e x p o sed in th e G a l l a t i n Range.
M a s t e r 's t h e s e s fro m M o n ta n a S t a t e
U n iv e r s ity have in c lu d e d c u rs o ry d e s c r i p ti o n s
th e
A rchean
T y sd a l,
rocks
1966).
in
th is
area
(M ifflin ,
A b r ie f d e sc rip tio n
and. l i m i t e d
1963;
W eber,
m apping o f
1965;
o f A rchean l i t h o l o g i e s
to
and
th e
s o u t h w e s t o f t h e s t u d y a r e a a c c o m p a n ie s a map o f t h e G a r n e t M o u n ta in
q u a d r a n g l e ( M c M a n n is a n d C h a d w i c k , 1 9 6 4 ) .
S p e n c e r an d K ozak (1975)
mapped an d d e s c r i b e d a p a r t o f t h e A r c h e a n r o c k s o f t h e G a l l a t i n Range
a l o n g t h e G a l l a t i n R i v e r Canyon a s w e l l a s t h e S p a n i s h P e a k s a r e a i n
t h e n o r t h e r n M a d iso n R ange.
G ile tti
(1966,
1968) and J a m e s and Hedge
(1980) h a v e r e p o r t e d a g e d a t e s f ro m t h e G a l l a t i n Canyon a r e a .
7
REGIONAL
The G a l l a t i n Range l i e s
A rchean P ro v in c e
(F ig u re I;
g e o l o g ic s e t t i n g
i n t h e n o r t h w e s t e r n p a r t o f t h e Wyoming
C o n d ie ,
1975).
Two f u n d a m e n t a l l y d i s t i n c t
t e r r a i n s e x i s t w i t h in th e A rchean b a s e m e n t o f t h i s
2).
(F ig u re
The N o r t h Snowy B lo c k i n t h e B e a r t o o t h Range l o c a l l y d e f i n e s t h e
b o u n d a r y b e t w e e n t h e s e tw o t e r r a i n s
east
p ro v in c e
of th is
b o u n d ary
(Mogk, e t a l ,
in rev iew ).
To t h e
t h e B e a r to o t h Range and o t h e r e x p o s u re s o f
A r c h e a n r o c k s a r e p r e d o m i n a n t l y com posed o f l a t e A r c h e a n a n d e s i t e s and
g r a n ito id s w ith in c lu s io n s of o ld e r s u p ra c r u s ta l rocks
1979; H e n ry , e t a l ,
th e
N o rth
1982;
M u e lle r, e t a l ,
1985).
Snowy B lo c k
p re d o m in a n tly
c o n sists
m eta sed im e n ta ry
rocks
V ita lia n o , et a l,
(S pencer
and K ozak,
1979; E r s l e v , 1983).
of
fo rm a tio n s.
p rese n t.
m a rb le s,
q u a rtz ite s,
M e ta -ig n e o u s
The t e r r a n e w e s t o f
1975;
of
h ig h -g ra d e
G a rih a n ,
1979;
T h ese ro c k s a r e com posed o f
q u a r t z o f e l d s p a t h i c g n e i s s e s and m e t a b a s i t e s ,
a m o u n ts
(P e te rm a n ,
as w e ll as su b o rd in a te
s illim a n ite
and u l t r a m a f i c
rocks
s c h is ts,
are
and
a lso
iro n
lo c a lly
The m e t a m o r p h ic g r a d e t h r o u g h o u t t h e s e e x p o s u r e s i n t h e
w e s t e r n t e r r a n e r a n g e s fro m g r e e n s c h i s t to g r a n u l i t e f a c i e s , w i t h
u p p e r-a m p h ib o lite
G a rih a n ,
1979;
g e n e ra tio n s
G a rih a n ,
fa c ie s
V ita lia n o ,
p red o m in an t
(S pencer
et a l,
E rsle v ,
1979;
o f f o ld in g have been re c o g n iz e d
1979;
V ita lia n o ,
et a l,
1979;
and
Kozak,
1983).
Two m a j o r
(S p e n c e r and K ozak,
E rsle v ,
1983).
1975;
1975;
The f i r s t
8
d e fo rm a tio n
c y c le
produced
iso c lin a l
fo ld s .
T hese
fo ld s
w ere
s u b s e q u e n t l y d e f o r m e d t o p r o d u c e l a r g e op en f o l d s .
J a m e s and Hedge (1980) r e p o r t e d R b - S r d a t a f ro m A r c h e a n r o c k s i n s o u t h w e s t M o n t a n a y i e l d i n g a 2 .7 5 B.Y. a g e d a t e f o r m e t a m o r p h i s m i n
th e
area.
G ille tti
(1966,
1968)
rep o rted
1.6 B.Y. a g e d a t e s
from
A rchean e x p o su re s w e s t o f t h e G a l l a t i n R iv e r, r e p r e s e n t i n g a r e g i o n a l
t h e r m a l e v e n t t h a t r e s e t K -A r i s o t o p i c c l o c k s .
A s h e a r zone in th e
P o r t a l C re e k a r e a o f t h e G a l l a t i n Range m a rk s t h e t r a n s i t i o n z o n e t h a t
se p a ra te s
th e
1.6 B.Y. t e r r a n e t o t h e n o r t h w e s t fro m a n o l d e r t e r r a n e
( " 2 . 7 B.Y.) t o t h e s o u t h e a s t . A t p r e s e n t n o a g e d a t e s y o u n g e r t h a n 2.1
B.Y. h a v e b e e n r e c o g n i z e d s o u t h e a s t o f t h e t r a n s i t i o n z o n e ( G i l e t t i ,
1966).
•U n c o n f o r m a b I y o v e r l y i n g t h e A r c h e a n b a s e m e n t i n t h e n o r t h e r n
G a lla tin
v o lca n ic s
R ange
are
P a leo z o ic
and
M eso zo ic
( F i g u r e 3;
C h a d w ic k ,
1969).
se d im e n ts
A rchean t e r r a n e s
M ontana h a v e b e e n e x p o s e d t h r o u g h C e n o z o ic b l o c k f a u l t i n g .
and E ocene
in so u th w e st
9
PETROLOGY
Q u a r tz o f e ld s p a th ic G neisses
The n o r t h e r n G a l l a t i n Range i s c o m posed p r e d o m i n a n t l y o f q u a r t z o —
f e ld s p a th ic g n e isse s.
The m a j o r i t y o f t h e s e g n e i s s e s e x h i b i t p r i m a r y
c o m p o s i t i o n a l l a y e r i n g on a c e n t i m e t e r - s c a l e .
These a re s tr o m a tic
m i g m a t i t e s , d e f i n e d by M c L e lla n (1983) a s m i g m a t i t e s w i t h a s m a l l s c a le lay e red s tr u c tu r e .
A m in o r am o u n t o f q u a r t z o f e l d s p a t h i c g n e i s ­
s e s e x h i b i t e v id e n c e o f leucosom e m o b il i z a t i o n .
d isc u sse d in a fo llo w in g s e c tio n .
These m ig m a tite s a r e
W ith t h e e x c e p t i o n o f t h e p r e s e n c e
o f e p i d o t e an d a m in o r am o u n t o f s i l l i m a n i t e , m o st o f t h e q u a r t z o f e l d s p a th ic g n e is s e s la c k b u lk c h e m ic a l c o m p o sitio n s n e c e s s a ry to g iv e
r i s e to index m in e ra ls .
F o rth c o m in g o b s e r v a t i o n s ,
h o w ever,
suggest
th a t th e g n e isse s i n i t i a l l y a tta in e d tr a n s it io n a l g r a n u lite fa c ie s
g rad e fo llo w e d by an ,e p id o te -a m p h ib e lite f a c i e s o v e r p r i n t.
F i e ld O ccu rren ce
Q u a rtz o fe ld s p a th ic g n e isse s
e x h ib it p e rv a siv e c o m p o sitio n a l la y ­
e rin g of m illim e te r to c e n tim e te r - s c a le , a lt e r n a t in g le u c o c r a tic ,
a m p h ib o le + b i o t i t e - r i c h ,
and h y b r id l a y e r s w i t h a s a l t and p e p p e r
a p p e a r a n c e ( d a r k m i n e r a l p e r c e n t a g e s a r e 1%, >10%, a n d 10%, r e s p e c ­
tiv e ly ).
C o m p o sitio n a l la y e r in g i s p a r a l l e l to m in e ra l f o l i a t i o n .
L e u c o c ra tic u n its occu r w ith in th e q u a rtz o f e ld s p a th ic g n e isse s as
c o n fo rm ab le
ro b la sts,
m il li m e t e r to c e n tim e te r - s c a le le n s e s , c o a le s c in g porphy-
and i s o l a t e d
in tra fo lia l
fo ld s.
10
M in e r a lo g y
M in e ra l
a s se m b la g e s
of
th e
q u a rtz o fe ld sp a th ie
q u a r t z i t e s a r e su m m arized in T a b le I.
se ctio n
are l is t e d
from t o n a l i t i c
d iag ra m
i n A p p e n d i x B.
to g r a n i t i c
fo r referen ce
a m p h ib o lite f a c ie s o v e rp rin t i s
h o rn b le n d e
(h b l) + / - p o ta s s iu m
g a r n e t (g t).
ite ,
C o m p o sitio n s p re d o m in a n tly range
on a S t r e c k e i s e n
The d o m in a n t a s s e m b l a g e o f t h e
q u artz
( q tz ) + p l a g i o c l a s e
(p la g ) + / -
f e ld s p a r (kspar) + b i o t i t e
A ccessory m in e r a ls in c lu d e m u sc o v ite ,
iro n -tita n iu m
o x id e p h a se s,
R etro g rad e phases in c lu d e s e r i c i t e ,
and
M odal a n a l y s e s o f e a c h t h i n
and h a v e b e e n p l o t t e d
(F ig u re 4).
g n e isse s
z irc o n ,
e p id o te , s illim a n -
a p a tite ,
c h lo rite ,
(b t) + / -
and t o u r m a li n e .
m u sc o v ite ,
c a lc ite ,
and
w h i t e m ic a m a t s .
T ita n iu m -ric h b i o t i t e g ra in s
(re d d ish -b ro w n p le o c h ro ism ) a re
s u g g e s t i v e o f h ig h m eta m o rp h ic g ra d e
a n tip e rth ite ,
are a lso
and m y r m e k i t i c
te x tu re s
p e rm issiv e of tr a n s itio n a l
(G u id o tti,
present
in
g ra n u lite
1977).
P e rth ite ,
some t h i n
fa c ie s
se ctio n s
c o n d itio n s.
P l a g i o c l a s e c o m p o s i t i o n s i n t h e q u a r t z o f e l d s p a t h i c g n e i s s e s r a n g e fro m
An2g ( o l i g o c l a s e ) t o A n ^
(an d e sin e). T hese c o m p o s itio n s a r e c o m p a t­
i b l e w i t h a s s e m b l a g e s fro m a m p h i b o l i t e t o g r a n u l i t e f a c i e s .
The r a n g e
i n c o m p o s i t i o n c o u l d r e f l e c t m ore t h a n o n e m e t a m o r p h ic g r a d e .
w as n o t o b s e rv e d in p l a g i o c l a s e g r a i n s .
Z oning
T he p r e d o m i n a n t a m p h i b o l e
p r e s e n t i s common h o r n b l e n d e ( e x t . $ = 1 3 ° - 3 2 ° , Z = o l i v e - g r e e n t o b l u e green,
(-),
2V=80o- 9 0 ° ) ,
a lth o u g h g r u n e r i te
( g ru n ) ,
g e d rite
(ged),
and
c u m m i n g t o n i t e (cumm) a r e p r e s e n t i n i s o l a t e d d i s c r e t e o c c u r r e n c e s .
C lin o p y ro x en es a r e d i o p s i d i c
(d io p ) t o s a l i t i c
(sal).
11
T ab le I.
N o te :
M i n e r a l a s s e m b l a g e s o f q u a r t z o f e l d s p a t h i c g n e i s s e s and
q u a rtz ite s.
P l a g i o c l a s e c o m p o s i t i o n s i n d i c a t e d w h e re d e t e r m i n a b l e .
A m p h ib o le - A b s e n t A s s e m b la g e s
q t z + b t + p la g f A n g g ) + k s p a r
q tz + b t + p lag + /- 'k s p a r + g t
q tz + p lag + k s p a r
q tz + b t + g t + p lag
A m p h i b o le - B e a r i n g A s s e m b la g e s
q tz + b t + g t + grun
q tz + b t + g t + plagfA n^g) + h b l
q t z + b t + p la g ( A n g ^ ) + k s p a r + h b l
p l a g + ged
P y r o x e n e - B e a r i n g A s s e m b la g e s
q t z + g t + p l a g (An^y) + h b l + s a l i t e
q tz + b t + p la g + h b l + dio p
Q u a rtz ite s
q t z + b t + g t + cumm
q tz + b t + g t + /- p lag
_
12
KEY
COMPOSITIONS
(from S t r e c k e i s e n ,
S= p r i m a r y c o m p o s i t i o n s
X= m o b i l i z e d m i g m a t i t e s
F ig u re 4.
1973).
I23456-
q u a rtz o lite (s ile x ite )
q u a rtz -ric h g ra n ito id s
g ran ite
g ra n o d io rite
to n a lite
q u a rtz m o n zo d io rite/
q u a r t z m onzogabbro
7- d io rite /g a b b ro /a n o rth o site
Q u a rtz o fe ld s p a th ic g n e is s c o m p o sitio n s.
F ie ld s are fo r
ig n e o u s r o c k s and a r e th u s f o r r e f e r e n c e o n ly .
P lo ts
r e p r e s e n t n o r m a liz e d m odal a b u n d a n c e s.
T h ree hundred
p o i n ts w ere c o u n te d f o r each p l o t .
13
R e t r o g r a d e A s s e m b la g e s
I n som e t h i n
Z = g re e n ish -b lu e ,
se ctio n s
(-),
h o rn b le n d e g r a i n s .
grade e f f e c ts .
h a stin g sitic
h o rn b le n d e
(ex t.
£ = 12°,
2 V = 6 0 ° ) o c c u r s a s p a t c h e s o r r i m s on comm on
T h is
o ccu rren ce
is
in te rp re te d
to
reflec t
re tro ­
E v i d e n c e o f r e t r o g r e s s i o n may r e f l e c t e i t h e r a g r e e n -
s c h is t o v e rp rin t or r e tro g ra d e p ro ce sse s a s s o c ia te d w ith th e in tro d u c ­
t i o n o f f l u i d s a lo n g f r a c t u r e zo n es.
re tro g ra d e
e v e n ts
o ccu rred
(e.g .
I t i s a lso p o s s ib le th a t se v e ra l
d u r in g th e w a n in g s t a g e s
of th e
t r a n s i t i o n a l g r a n u lite a n d /o r e p id o te -a m p h ib o lite f a c i e s c o n d itio n s or
t h a t a c o m b in a tio n of c a u se s im p a rte d retro g rad e e ffe c ts ).
S ev eral
o th e r m ic ro sc o p ic o b s e rv a tio n s of re tro g ra d e e f f e c ts fo llo w .
Some
e p i d o t e g r a i n s h a v e b e e n o b s e r v e d t o o c c u r b e t w e e n b i o t i t e and h o r n ­
b len d e g ra in s
re a c tio n :
as p ro d u c ts
of re tro g re ssio n ,
h b l + K+ = b t + c l i n o z o i s i t e .
degrees of a l t e r a t i o n to c h l o r i t e ,
phases.
c h a r a c t e r i z e d by th e
B io tite
e x h ib its v a ry in g
m u s c o v i t e , and i r o n - t i t a n i u m
S a g e n i t i c t e x t u r e s a r e fo u n d r a r e l y ,
o x id e
d e fin e d as r u t i l e need­
l e s a r r a n g e d a l o n g t h e p s e u d o - h e x a g o n a l s y m m e tr y o f b i o t i t e .
S e ric ite
o c c u r s a s a common a l t e r a t i o n p r o d u c t o f p l a g i o c l a s e .
T ex tu res
O n ly
one
fo lia tio n
q u a rtz o fe ld sp a th ic
su rface
g n e isse s.
It
has
is
been
id e n tifie d
d e fin e d
by th e
w ith in
a lig n m e n t
th e
of
b i o t i t e g r a i n s , n e m a t o b l a s t i c a m p h i b o l e s , c o lu m n a r s i l l i m a n i t e , l i n e a r
iro n -tita n iu m
g ra in s.
o x id e g r a i n s ,
ovoid g a r n e t s ,
and some e l o n g a t e q u a r t z
G r a i n s i z e s r a n g e f r o m f i n e - m e d i u m (Imm) t o c o a r s e (>3mm).
Changes in
g ra in
siz e
are
p rese n t w ith in
in d iv id u a l
c o n fo rm ab le
14
lay e rs.
T h i s m ay r e f l e c t e i t h e r g r a i n s i z e d i f f e r e n c e s
present
in
th e
m eta m o rp h ism .
p ro to lith
or
d iffe re n tia l
c ry sta l
t h a t w ere
g ro w th
V a ry in g d e g re e s o f t e x t u r a l e q u i l i b r i u m
o b serv ed in th in s e c tio n .
d u rin g
have been
C u rv ed , s e r r a t e d , em bayed, and s t r a i g h t
g ra in b o u n d aries as w e ll as t r i p l e
j u n c t i o n s have a l l
been o bserved.
G ra n o b la stic te x tu r e s a re lo c a lly p re s e n t.
D e f o r m a t i o n a l and R ecr y s t a l l i z a t i o n E f f e c t s
S t r a i n i s m ic r o s c o p i c a l ly e v id e n t i n v a r io u s fo rm s th ro u g h o u t th e
q u a rtz o fe ld s p a th ic g n e isse s.
stra in .
th e
Q u a r tz g r a i n s e x h i b i t v a r y i n g d e g r e e s o f
R e c r y s t a l l i z a t i o n i s common a s w e l l a s e v i d e n c e o f s t r a i n i n
fo rm
of
su b g ra in s,
re d u c tio n s
in
g ra in
s iz e ,
and
u n d u lo se
e x t i n c t i o n s i m i l a r t o t e x t u r e s r e p o r t e d b y M i t r a , 1978, V auchez, 1980,
W h ite , e t a l ,
1980, and T u l l i s , e t a l ,
a ls o been o b serv ed .
som e e x h i b i t i n g
e x tin c tio n ,
mon.
P la g io c la se
reco v ery
1982).
r a n g e s fro m w e l l - r e c r y s t a l l i z e d t o
stru c tu re s
such as
and i n c i p i e n t p o l y g o n i z a t i o n .
P la g io c la se g rain s
R ib b o n t e x t u r e s h av e
su b g ra in s,
u n d u lo se
D e f o r m a t i o n t w i n s a r e com­
o c c u r b o t h a s ro u n d e d p o r p h y r o b l a s t s and a s
s m a l l e r n e o b l a s t s i n t h e g ro u n d m a s s .
M arked r e d u c t i o n i n g r a i n s i z e s
in th e m a trix su rro u n d in g p la g io c la s e p o rp h y ro b la s ts is p re s e n t in
s o m e s a m p l e s . Some b i o t i t e g r a i n s s h o w e v i d e n c e o f s t r a i n t h r o u g h
s tr o n g ly un d u lo se e x tin c tio n , unequal p le o c h r o is m
ragged form , o r b e n t g r a in s .
and b i r e f r i n g e n c e ,
B i o t i t e i s c o m m o n ly s y n k i n e m a t i c a n d
o c c u r s a s f o l i a t e d u n s t r a i n e d and w e l l - r e c r y s t a l l i z e d g r a i n s .
t a l l i z a t i o n p ro c e sse s o u tla s te d d e fo rm a tio n a l e f f e c ts .
R ecrys­
15
In sum m ary, m o st o f th e q u a r t z o f e l d s p a t h i c g n e i s s e s a r e o f t h e
e p id o te -a m p h ib o lite
fa c ie s.
H ow ever,
it
is
b e lie v e d
th at
th e se
g n e is s e s o r i g i n a l l y a tt a in e d t r a n s i t i o n a l g r a n u l i te f a c i e s grade based
on t h e p r e s e n c e o f g r a n o b l a s t i c
in d ic a tiv e
of
th a t
g rade.
B ased
m e t a b a s i t e s and t h e o b s e r v a t i o n
e v id e n t w ith in
te x tu re s
th at
on
and m i n e r a l
fo rth c o m in g
a sse m b la g e s
e v id e n c e
no new s t r u c t u r a l , e l e m e n t s
fro m
are
th e e p id o t e - a m p h ib o l it e f a c ie s ro ck s, i t is b e lie v e d
t h a t a t r a n s i t i o n a l g r a n u l i t e f a c i e s o l d e s t e v e n t w as s u b s e q u e n tly
o v e r p r i n t e d by e p i d o t e - a m p h i b o l i t e f a c i e s c o n d i t i o n s .
P ro to lith
D ue t o t h e h i g h g r a d e o f m e t a m o r p h i s m a t t a i n e d a n d e x p o s u r e t o
in te n s e d e fo rm a tio n ,
been o b lite r a te d .
an y r e l i c t
s e d im e n ta ry o r ig n eo u s t e x t u r e s have
A l l u n i t s a r e c o n f o r m a b l e and o c c u r on a m i l l i m e t e r
to c e n tim e te r - s c a le of la y e rin g .
T h e r e a r e no d i s c e r n a b l e s p a t i a l
r e l a t i o n s h i p s a m o n g s t t h e d i f f e r e n t q u a r t z o f e l d s p a t h i c g n e i s s c o m p o s i­
tio n s
(i.e .
c e rta in
i n d i v i d u a l l i t h o l o g i e s do n o t a p p e a r t o b e c o n c e n t r a t e d i n
areas).
The r a n g e o f s t u d y a r e a q u a r t z o f e l d s p a t h i c g n e i s s
c o m p o s i t i o n s h a s b e e n p l o t t e d on a S t r e c k e i s e n d i a g r a m
( F i g u r e 4 ).
P o ta ssic
se g re g a tio n s y ie ld
g ra n itic
fo r referen ce
c o m p o sitio n s.
Com­
p o s itio n s of q u artzo f e ld sp a th ic ban d ed g n e is s e s p r e d o m in a n tly ran g e
f ro m t o n a l i t i c ' t o
g ra n itic .
N o ta b le e x c e p tio n s p l o t w i t h i n
th e f o l ­
l o w i n g f i e l d s on t h e S t r e c k e i s e n d i a g r a m .
Quartz-rich Granitoid and Quartzolite Compositions.
known ig n e o u s ro c k s w i t h c o m p o s itio n s t h i s q u a r t z r i c h .
T h e r e a r e no
Two o f t h e
r o c k s t h a t p l o t i n t h i s a r e a a r e m y l o n i t e s com posed o f m o re t h a n 75%
16
q u a rtz .
These ro ck s l i k e l y
q u a r tz - r ic h san d sto n es.
ite ,
r e p r e s e n t m e ta m o rp h ic e q u i v a l e n t s of
One q u a r t z - r i c h g r a n i t o i d
c o n ta in s
sillim a n -
s tr o n g ly in d ic a ti v e of a se d im e n ta ry o r ig in .
Rocks p l o t t i n g
Diorite/Gabbro/Anorthosite.
on F i g u r e 4 w i t h
t h e s e c o m p o s i t i o n s may r e p r e s e n t p r i m a r y c o m p o s i t i o n s o f d a c i t e ,
d io rite ,
or
p la g io c la s e arkose,
m o r p h ic d i f f e r e n t i a t i o n
M yers (1978) h a s
o r s e g r e g a t i o n s r e s u l t i n g fro m m e t a ­
or a n a te x is.
su g g e ste d t h a t u n ifo rm ly banded g n e is s e s in
W est G r e e n l a n d r e s u l t e d f ro m e x t r e m e f l a t t e n i n g o f p l u t o n i c r o c k s t h a t
m ig h t have o t h e r w i s e b een o v e rlo o k e d a s l i t t l e d eform ed r e l i c t p rim a ry
la y e rin g .
G n e i s s i c b a n d i n g due t o
p lu to n ic
rocks
d e m o n stra te d
for
a n d /o r
in te n s e d efo rm atio n
m e ta m o rp h ic
sev eral
h ig h -g ra d e
w i d e s p r e a d e x t e n t i n W est G r e e n la n d
et
a l,
1973).
H ow ever,
sev eral
(e.g.
of o rig in a lly
d iffe re n tia tio n
has
g ra n itic
u n its
g n e iss
M cGregor,
1973;
o b se rv a tio n s
of
been
of
B rid g w a te r,
s tu d y
area
q u a r t z o f e l d s p a t h i e g n e i s s e s do n o t s u p p o r t a p l u t o n i c o r i g i n :
1.
A p l u t o n i c p a r e n t w o u ld y i e l d
r o c k s m o re m i n e r a l o g i c a l l y
homogenous t h a n t h o s e o b s e r v e d i n t h e s t u d y a r e a ;
2.
B i o t i t e an d h o r n b l e n d e a r e l o c a l l y p r e s e n t i n g r e a t e r a m o u n ts
th a n w o u ld be e x p e c te d fro m a c a l c - a l k a l i n e ig n e o u s p a r e n t
rock;
3.
Igneous ro ck s la c k t y p i c a l l y p e l i t i c
and s i l l i m a n i t e .
m in e ra ls such as g a rn e t
B o th m i n e r a l s a r e p r e s e n t i n s tu d y a r e a
q u a r t z o f e ld s p a t h ic g n e is s e s ; g a r n e ts a re a b u n d a n t.
I n l i g h t o f t h e a b s e n c e o f any r e a d i l y o b s e r v a b l e i n d i c a t i o n s o f
an i g n e o u s o r i g i n s u c h a s d i s c o n f o r m ah I e l a y e r i n g ,
r e l i c t ig n e o u s
17
tex tu res,
c le a r
o r c o m p le x o s c i l l a t o r y
th a t
tra c e
e le m e n t
z o n in g i n p l a g i o c l a s e g r a i n s ,
and o t h e r g e o c h e m ic a l
a n a ly se s
it
is
m ust be
i m p l e m e n t e d i n o r d e r t o r e s o l v e t h i s p r o b le m .
A n o th e r
c o m p o sitio n s
sed im e n ta ry
p o s s ib ility
rep resen t
o rig in .
is
th a t
th e
a su p ra c ru sta l
F e a tu re s
w ith in
to n a litic
and
g ra n itic
sequence of p re d o m in a n tly
th e
q u a rtz o fe ld sp a th ic
g n e isse s
t h a t a re s u g g e s tiv e of a se d im e n ta ry o r ig i n in c lu d e :
1.
The p r e s e n c e o f s i l l i m a n i t e ;
2.
The p r e s e n c e o f q u a r t z i t e u n i t s ;
3.
A c o n c o r d a n c e o f u n i t s w i t h s c h i s t s and t h i n s h e e t s o f a m p h i­
b o lite ;
4.
A p e rs is te n c e of lay e rin g ;
5.
The p r e s e n c e o f a g r a d u a l r e p e t i t i o n o f c o m p o s i t i o n a l l a y e r s
m ost l i k e l y
r e p r e s e n ts p rim a ry c o m p o s itio n a l la y e rin g
m e t a m o r p h ic d i f f e r e n t i a t i o n
as
i s n o t e x p ected t o g e n e ra te t h i s
p a tte rn ;
6.
The p r e s e n c e o f d i s c o n t i n u o u s q u a r t z o f e l d s p a t h i c l a y e r s on a
m illim e te r-to c e n tim e te r-sc a le
may r e p r e s e n t p r i m a r y i n t e r ­
b e d d in g o f s e d im e n ta ry u n i t s .
Some o f t h e a b o v e c r i t e r i a h a v e b e e n c i t e d by n u m e ro u s a u t h o r s i n
p o stu la tin g
a sed im e n ta ry o r ig in
for
th e
q u a rtz o fe ld sp a th ic
i n A r c h e a n e x p o s u r e s i n s o u t h w e s t M o n ta n a (e.g. C o rd u a ,
and K ozak,
1975; V i t a l i a n o ,
and W ils o n , 1981).
(HI) o f f e r s
et a l,
g n e isse s
1973;
Spencer
1979; F o u n t a i n a n d D e s m a r a i s ,
1980;
An o u t c r o p a l o n g H y a l i t e C r e e k i n t h e s t u d y a r e a
th e s tro n g e s t f ie ld
e v id e n c e f o r a s e d im e n ta ry
o rig in
of
t h e g n e i s s e s . A m in o r am ount o f c e n t i m e t e r - s c a l e s c h i s t u n i t s a r e
18
in tim a te ly
g n e is s e s
and
and
c o n fo rm ab ly
m e ta b a site
q u a rtz o fe ld sp a th ic
in te rb e d d e d
u n its.
g n e isse s
is
w ith
q u a rtz o fe ld sp a th ic
L a y e rin g
th o u g h t
to
in
m ost
of
rep resen t
th e
p rim a ry
c o m p o s i t i o n a l l a y e r i n g , t h o u g h i t l i k e l y h a s b e e n m o d i f i e d t o som e
d e g re e by t r a n s p o s i t i o n
a n d / o r m e t a m o r p h ic d i f f e r e n t i a t i o n .
P a rtia l
m e ltin g is su g g e ste d in m ig m a titic g n e is s e s to be d isc u s s e d in th e
n e x t sectio n .
One e x p l a n a t i o n
S tre c k e ise n
d iag ra m
fo r th e
d istrib u tio n
(F ig u re
4)
m ay
o f c o m p o s i t i o n s on t h e
be
as
fo llo w s.
T o n a litic
c o m p o s i t i o n s f o r s t u d y a r e a m e t a s e d i m e n t s may r e f l e c t t h e N o r t h Snowy
B lo c k o f t h e B e a r t o o t h Range a s a s o u r c e a r e a .
tro n d h je m itic
T h is i s re a s o n a b le as
r o c k s t h e r e a r e o f a p p r o p r i a t e c o m p o s i t i o n and a g e (~3.5
Ga, Mogk, 1984, and Mogk, e t a l ,
in rev iew ).
g ra n itic
et a l,
c o m p o sitio n
(M u e lle r,
P o ta s s iu m -ric h rocks of
1 9 8 2 ) may r e f l e c t , t h e l a t e r
c a l c - a l k a l i n e r o c k s o f t h e B e a r t o o t h Range a s t h e i r s o u r c e .
Though t h e r e
is
no u n e q u i v o c a l
e v id e n c e o f an o r i g i n ,
fie ld
o b s e r v a t i o n s , p e t r o g r a p h i c s tu d y , and c o r r o b o r a t i v e e v id e n c e fro m
p rev io u s
stu d ie s
of
su rro u n d in g
ranges
m ost
stro n g ly
p red o m in an tly se d im e n ta ry o r ig in f o r q u a r t z o f e l d s p a t h i c
th e re g io n .
ark o ses.
to
th e
c o m p o sitio n .
g n e isse s
a
in
r e p r e s e n t m eta g ra y w a c k e s o r m e ta -
Some am ount o f a c i d v o l c a n i c l a s t i c
c o n trib u te d
t o n a l i t ic
These ro ck s l i k e l y
sup p o rt
su p ra c ru sta l
p ile
s e d i m e n t s may a l s o h a v e
th at
y ie ld e d
g n e isse s
of
19
M ig m a tite s
U n iq u e o c c u r r e n c e s o f m i g m a t i t e a r e e x h i b i t e d w i t h i n t h e L e v e r i c h
C re e k o u t c r o p
(L—I ) .
T h e s e m i g m a t i t e s d i f f e r fro m t h e p r e d o m i n a n t l y
s t r o m a t i c m ig m a tite s o f t h e s tu d y a r e a in t h a t leu co so m es w i t h i n th e
L e v e r i c h C re e k m i g m a t i t e s h a v e b e e n m o b i l i z e d ,
th u s in d ic a tin g su p er­
h e a t e d c o n d i t i o n s w i t h r e s p e c t t o t h e s t r o m a t i c m i g m a t i t e s (T racy and
R o b in s o n ,
1983).
o b serv ed .
fea tu re s
Two o c c u r r e n c e s
o f m o b iliz e d
m ig m a tite s have been
No s i n g l e m e c h a n i s m c a n a c c o u n t f o r a l l o f t h e o b s e r v e d
d is p la y e d by th e s e
m ig m a tite s.
T h e i r d e s c r i p t i o n and p e t r o -
g en esis w i l l be d isc u sse d s e p a ra te ly .
The f i r s t o c c u r r e n c e o f m o b i l i z e d
g n e iss
m ig m a tite l i e s w i t h in a m afic
c h a r a c t e r i z e d by th e a sse m b la g e q tz + g t + h b l + p la g
s a l + e p id o te .
(An^y) +
T h i s r o c k u n i t i s t h o u g h t t o b e a m eso so m e, s i m i l a r t o
t h a t d e s c r i b e d b y M c L e lla n (1983) a s a n u n m i g m a t i z e d b o d y o c c u r r i n g
w ith in a m ig m a titic s u ite .
The l e u c o s o m e s w i t h i n t h i s g n e i s s a r e
c h a r a c t e r i z e d by t h e a sse m b la g e q tz + p la g
L e u c o so m e s o c c u r a s c e n t i m e t e r - s c a l e
(An^g) + m i c r o c l i n e + / - b t .
lay ers,
some p t y g m a t i c i n f o rm .
They a r e p r e d o m i n a n t ly c o n f o r m a b le w i t h th e s u r r o u n d in g g n e is s b u t
a lso
occur as ir r e g u la r ly
ro u g h ly co n fo rm ab le
fo rm ed , c e n ti m e t e r - s c a le m asses,
(F ig u re 5).
The i r r e g u l a r f o rm i s
h i g h g r a d e m e t a m o r p h ic c o n d i t i o n s
(J o h a n n e s and G u p ta ,
still
l i k e l y due t o
1982).
C ross­
c u t t i n g l e u c o s o m e l a y e r s a r e r a r e a n d o c c u r on a v e r y l o c a l ( c e n t i ­
m e t e r ) s c a l e . The l a c k o f s t r o n g l y a n i s o t r o p i c p a t t e r n s w i t h i n t h e
leucosom es i s
is
s u g g e s tiv e o f a n o n -ig n e o u s o r i g i n
(Y ard ley ,
1978).
It
a l s o b e l i e v e d t h a t t h i s l e u c o s o m e w a s n o t d e r i v e d v i a m e ta m o r p h ic
se g re g a tio n
as
th e re
is
not
a
c lo se
re la tio n sh ip
b e tw e e n
its
20
mafic gneiss
F ig u re 5.
M o b i l i z e d l e u c o s o m e s (L) w i t h i n m a f i c g n e i s s (mesosome).
L en s c a p (C) d i a m e t e r = 5 cm.
p l a g i o c l a s e c o m p o s i t i o n (An^g) and t h e p l a g i o c l a s e c o m p o s i t i o n i n
th e su rro u n d in g g n e iss
(An^y).
Y a r d l e y , 1978, d e f i n e s c l o s e a n o r t h i t e
c o m p o s i t i o n s a s t h o s e w i t h i n a few p e r c e n t o f e a c h o t h e r .
s u r r o u n d i n g t h e l e u c o s o m e a t one t i m e a t t a i n e d
g r a n u lite g rade.
le a st
re la tio n sh ip
m e l t i n g and g r a n u l i t e f a c i e s c o n d i t i o n s
S in ce th e leucosom e p l a g i o c l a s e
b e tw e e n p a r t i a l
( e .g . F y f e ,
c o m p o sitio n
1973; W in k le r,
is
m ore a l b i t e - r i c h t h a n t h e p l a g i o c l a s e o f t h e m esosom e,
t h a t in s i t u p a r t i a l m e ltin g (W in k ler,
P la te n ,
1961) i s
m o b iliz a tio n
of
tra n sitio n a l
T h is g rad e i s c o m p a tib le w ith a n a te x is as i t has
been su g g ested t h a t th e r e i s a g e n e t i c
1976).
at
G n e isse s
sig n ific a n tly
i t is b e lie v e d
1961, 1979; a n d W i n k l e r and Von
t h e m ost r e a s o n a b le o r i g i n f o r t h i s m ig m a tite .
th e se
leu c o so m es
is
in d ic a tiv e
of
h ig h
The
grade
21
m etam orphic c o n d itio n s .
I t i s i n f e r r e d by t h i s a u t h o r t h a t p a r t i a l
m e ltin g took p lace a t t r a n s i t i o n a l g r a n u l i t e f a c i e s c o n d itio n s .
The s e c o n d o c c u r r e n c e o f m i g m a t i t e o c c u r s a s c e n t i m e t e r - s c a l e ,
u n co n fo rm ab le, n o n - d i r e c t io n a l leucosom es w ith in m e ta b a s ite u n i ts
(Figure 6) t h a t are d isc o n tin u o u s but conform able w ith surro u n d in g
gneisses.
Leu co so mes
locally cross-cut
the m etabasite.
Local t ig h t
t o i s o c l i n a l f o l d i n g o f t h e l e u c o s o m e o c c u r s on a c e n t i m e t e r - s c a l e .
T h i s m i g m a t i t i c l e u c o s o m e c o n t a i n s s u b s t a n t i a l l y more m i c r o c l i n e t h a n
the p rev io u sly d escrib ed
leucosom es.
On t h i s
b asis,
the
differen tiated .
30 cm
Figure 6 .
N o n - d i r e c t i o n a l le u c o s o m e w i t h i n m e t a b a s i t e u n i t .
two a r e
22
The f o l l o w i n g
ob serv atio n s
im p ly th a t the leu c o c ra tic m ate ria l
was l o c a l l y .i n t r o d u c e d f ro m an e x t e r n a l s o u r c e on an o u t c r o p s c a l e :
1.
M elanosom e u n i t s
are
leu co cratic u n its.
It
is
p o ssib le
lo cally
in v a d e d and a s s i m i l a t e d
by
Some m e l a n o s o m e s a p p e a r t o b e r o t a t e d .
th at
the
leucosom e
rep resen ts
a late
h y d r o t h e r m a l d e p o s i t , i n f i l l i n g a r o u n d t h e melanosome; .
2.
Th e m i n e r a l p h a s e s i n t h e l e u c o s o m e a r e n o t r e l a t e d t o t h e
m ineralogy of th e h o st rock;
3.
Melano so mes t h a t c o n t a i n t h e m i g m a t i t i c l e u c o s o m e e x h i b i t t h e
fo llo w in g c h a r a c t e r i s t i c s t h a t imply a l t e r a t i o n :
a.
H a s t i n g s i t i c p a t c h e s w i t h i n common h o r n b l e n d e g r a i n s ;
b.
A m a j o r amount o f c h l o r i t e
o ccu rs as pseudomorphs a f t e r
b i o t i t e and i n p l a c e s h o r n b l e n d e i s r e p l a c e d by c h l o r i t e ;
c.
E pidote
occurs
as
a replacem ent
of
calcite
w ith
and
w ithout c h lo r i te .
In
ad d itio n ,
ex ten siv e
p lag io clase
sericitizatio n
th ro u g h o u t th e leucosom e, ag ain i n d i c a t i n g a l t e r a t i o n .
occurs
E xtensive
re p la c e m e n t o f p l a g i o c l a s e by m i c r o c l i n e has been observed th roughout
t h e l e u c o s o m e . S i m i l a r o b s e r v a t i o n s h a v e b e e n r e p o r t e d i n t h e Tobacco
Root Range and a r e a t t r i b u t e d
1973).
to a p o t a s s i c m o b iliz a tio n
(Cordua,
Hydrotherm al a l t e r a t i o n , perhaps r e s u l t i n g from e x te r n a l m eta­
som atism ,
i s s t r o n g l y s u g g e s t e d by t h e e x t e n s i v e amou nt o f a l t e r a t i o n
observed.
D etailed
petrographic
and e x p e r i m e n t a l d a t a a r e n e c e s s a r y f o r a
c le a r e r understanding of m igm atite genesis
studies
are
beyond
the
scope
of
th is
in th e study area.
thesis.
N o n etheless,
These
the
23
o b s e r v a t i o n s made s e r v e a s a f i r s t a p p r o x i m a t i o n and a s a s p r i n g b o a r d
for fu rth e r investigation.
Based on t h e p r e c e e d i n g d i s c u s s i o n and on
t h e amou nt o f d a t a a v a i l a b l e , t h i s a u t h o r s p e c u l a t e s t h a t t h e L e v e r i c h
Creek m i g m a t i t e s
i n t h e c o n f o r m a b l e and n o n - d i r e c t i o n a l leucosomes
resu lted
situ
from
in
p artial
m elting
and
ex tern al
m etasom atic
processes, respectively.
Am phibolite F a c ie s M etab asites
Most m e t a b a s i t e s w i t h i n t h e s t u d y a r e a a r e o f t h e a m p h i b o l i t e
f a c i e s o f E s k o la (1939), d e f i n e d as t h a t f a c i e s i n w h ic h b a s i c r o c k s
a r e r e p r e s e n t e d by h o r n b l e n d e - p l a g i o c l a s e a sse m b la g e s w i t h p l a g i o c l a s e
c o m p o s i t i o n s more c a l c i c t h a n AngQ.
F i e ld Occurrence
F ie ld occurrences of th e am phibolite fa c ie s m etab asites occur in
th e fo llo w in g v a r i e t y of forms:
1.
As g r a d a t i o n a l m i l l i m e t e r t o c e n t i m e t e r - s c a l e c o n f o r m a b l e
la y e rs w ith in q u a rtz o fe ld sp a th ic gneisses;
2.
As c e n t i m e t e r and m e t e r - s c a l e l e n s - s h a p e d p o d s ;
3.
As m e t e r - s c a l e s p h e r o i d a l I y w e a t h e r e d c a t a c l a s t i c p o d s .
M ineralogy
M i n e r a l a s s e m b l a g e s a r e s u m m a r i z e d i n T a b l e 2.
of
each
th in
section
are
listed
in
Appendix
assem blage i s hbl + p lag + /- qtz + /- b t + /- g t.
include iro n -tita n iu m
oxides,
zircon,
sphene,
M ineral contents
C.
The
dom inant
A ccessory m in erals
and a p a t i t e .
Retrograde
p h a s e s i n c l u d e c h l o r i t e , s e r i c i t e , p r e h n i t e , e p i d o t e , and s a g e n i t i c
24
Table 2.
Note:
Am phibolite f a c i e s m e ta b a s ite assem blages.
P l a g i o c l a s e co m p o sitio n s i n d i c a t e d where d e te r m i n a b le .
Dominant A s s e m b l a g e s
hbl + p lag + q tz + g t + diop
hbl + p lag (^ 0 ) + qtz
hbl + plag + qtz + b t + s a l
h b l + p la g + b t +qtz
h b l + p l a g (5 ^) + b t
hbl + p l a g (20) + b t + g t
hbl + plag + g t + s a l
h b l + p l a g (7 3 ) + g t + b t + q t z
hbl + plag + gt + qtz
hbl + plag X ^) + sal
Un iq ue V a r i e t i e s
actin o lite + bt
cumm + t r e m + p l a g + q t z + g t
ru tile
after bio tite.
Main a s s e m b l a g e and r e t r o g r a d e p h a s e s f o r t h e
am phibolite fa c ie s m etabasites are i l l u s t r a t e d
common t o b o t h m a f i c
rocks
i n F i g u r e 7.
and t h e q u a r t z o f e l d s p a t h i c
M inerals
g n e is s e s have
been p re v io u s ly de scrib ed in th e q u a rtz o fe ld s p a th ic g n e iss se ctio n .
P l a g i o c l a s e c o m p o s i t i o n s r a n g e f r o m AngQ ( o l i g o c l a s e ) t o Anyg
(bytow nite), c o n s is t e n t w ith u p p e r - a m p h i b o l i t e f a c i e s
the q u artzo feld sp ath ic gneisses,
common h o r n b l e n d e (
rocks.
As i n
th e predom inant amphibole p re s e n t i s
e x t . $ =13° - 3 2 ° , z = o l i v e g r e e n t o b l u e g r e e n .
Figure 7
A
A
diop
D o m in a n t
stable a ss em b lag e
Retrograde
phases
ACF d i a g r a m s i l l u s t r a t i n g d o m in a n t s t a b l e and r e t r o g r a d e p h a s e a s s e m b l a g e s i n s t u d y
area am phibolite fa c ie s m e ta b a s ite s .
26
2V = 8 0° - 9 0° ).
Foliated
tecto n ically .
and l i n e a t e d h o r n b l e n d e s m u s t h a v e f o r m e d s y n -
In one t h i n
section,
a m icro-scale is o c lin a l sim ila r
f o ld composed of p o ly g o n a l a rc s of a x i a l p l a n a r h o rn b le n d e g r a in s
d e f i n i n g a s e c o n d s —s u r f a c e i s p r e s e n t .
p rovide
ad d itio n al
cry stallizatio n
evidence
histo ry
for
observed c o n ta in in c lu s io n s
sent in the
later
rock,
for
a
the
h ornblendes.
( -,
syn tecto n ic
of q u artz,
or
p o st-tecto n ic
Many
plagioclase,
ext.
hornblende g ra in s .
$ = 1 2° ,
Patches
2V=60°,
or rim s
and b i o t i t e p r e ­
of h a s tin g s itic
z = g r e e n i s h b l u e ) o c c u r on common
H a s t i n g s i t i c hornblende a ls o t y p i c a l l y occurs
a l o n g c l e a v a g e s and c r a c k s w i t h i n t h e s e g r a i n s .
H a s t i n g s i t e was n o t
o b s e r v e d t o o c c u r a l o n g a n y d e f i n a b l e new s - s u r f a C e s .
ex h ib its
hornblendes
i n d i c a t i n g t h a t t h e h o r n b l e n d e s g r ew w i t h o r a t a
sta g e than th o se m in e rals.
hornblende
The p o l y g o n a l a r c g r a i n s
alteratio n
to c h l o r i t e
or b io tite
H ornblende
i n some t h i n s e c t i o n s .
Clinopyroxene c om positions a re d io p s id ic to s a l i t i c .
Textures
G r a i n s i z e s r a n g e f ro m f i n e (.5mm and l e s s ) t o m e d i u m - c o a r s e (35mm).
L a y e rin g o c c u rs from a m i l l i m e t e r t o p r e d o m i n a t ly c e n t i m e t e r -
s c a l e and a l t e r n a t e s w i t h q u a r t z o f e l d s p a t h i c
gneisses.
The two p r e ­
dominant t e x t u r e s in th e a m p h ib o lite f a c i e s m e t a b a s i te s a re :
to b lastic
h o r n b l e n d e w i t h i n t e r s t i t i a l x e n o b l a s t i c p l a g i o c l a s e and
q u a r t z , a n d 2) g r a n o b l a s t i c .
layering
I) n e m a -
F o l i a t i o n i s d e f i n e d by c o m p o s i t i o n a l
in clu d in g n e m a to b la stic hornblende,
an a l i g n m e n t Of b i o t i t e
g r a i n s , and f l a t t e n e d q u a r t z i n some t h i n s e c t i o n s .
M ineral l i n e a -
t io n s w ere u s u a lly too f in e to a llo w m easurem ent in th e f i e l d .
A ll
27
d e g r e e s o f r e c r y s t a l l i z a t i o n , s t r a i n r e c o v e r y , and g r a i n shape a r e
present.
grains
Some t h i n
w ithin
the
same t h i n
recry stallizatio n .
still
sections
display
sections,
Most e x h i b i t
in itial
recry stallized
and s t r a i n e d
in d ic a ti n g v a ry in g degrees of
te x tu r a l adjustm ent but
are
t e x t u r a l l y i n e q u i l i b r a t e d b a s e d on t h e l a c k o f t r i p l e j u n c t i o n s
b e t w e e n g r a i n s and t h e p r e s e n c e o f c u r v e d t o s e r r a t e d g r a i n b o u n d a r i e s
of v ario u s m inerals.
Unique O ccurrences
Two u n i q u e o c c u r r e n c e s o f a m p h i b o l i t e f a c i e s m e t a b a s i t e s o c c u r
w i t h i n a H y a l i t e Creek o u tcro p (H -l).
this
outcrop i s
W ith th e e x c e p t io n of t h e s e ,
composed p r e d o m i n a n t l y o f c o n f o r m a b l e p l a n a r q u a r t z o -
fe ld s p a th ic u n its th a t are g ra d a tio n a lly interbedded w ith m etabasites
on a m i l l i m e t e r t o c e n t i m e t e r - s c a l e .
The f i r s t u n i q u e o c c u r r e n c e o f m e t a b a s i t e a t t h e H y a l i t e C r e e k
outcrop
(H-l) i s
a m e t e r - s c a l e pod t h a t o c c u r s
quartzof eld sp ath ic
gn eiss
u n its
(F igure
8 ).
in sharp co n tact w ith
The pod a p p e a r s
to
e x h i b i t i n t e r n a l f l o w o r f o l i a t i o n when s e e n i n o u t c r o p . However, t h i s
body i s i n s u f f i c i e n t l y e x p o s e d t o e n a b l e d i s c e r n a b l e
of
its
stru ctu re.
This
rock
unit
assem blage hbl + p lag + s a l i t e .
g ran o b lastic.
characterized
by
the
m ain
One w e l l - d e v e l o p e d c o m p o s i t i o n a l
f o l i a t i o n i s expressed in t h i s rock,
sically
is
characterization
though th e m ic r o te x tu r e i s c l a s ­
T h e r e a r e some i r r e g u l a r l y - s h a p e d p l a g i o c l a s e
p o r p h y r o b l a s t s w i t h i n t h i s ro ck , th o u g h m ost of th e p l a g i o c l a s e i s
recry stallized .
islands
H o rn b le n d e and s a l i t e g r a i n s t e n d t o form s u b t l e
s u r r o u n d e d by p l a g i o c l a s e .
A m i n o r amount o f
salite
c lu m ps
28
I meter
Figure 8 .
Pod ( c r o s s - h a c h u r e d p a t t e r n ) i n
q u a r t z o f e l d s p a t h i c g n e is s e s (qf g n ) .
sharp
co n tact
w ith
29
a r e s u r r o u n d e d by h o r n b l e n d e .
H o r n b l e n d e p a t c h e s common w i t h i n s a l i t e
g r a i n s a r e s u g g e s t i v e o f t h e r e a c t i o n h b l c px + q t z + p l a g .
T r e m o l i t e - c u m m i n g t o n i t e c a t a c l a s t i c pods o c c u r w i t h i n t h e H y a l i t e
Cree k o u t c r o p (H-I) a s m e t e r - s c a l e s p h e r o i d a l l y w e a t h e r e d p o d s t h a t
l i e w i t h i n a h i g h l y w e a t h e r e d zo n e ( F ig u r e 9).
The m i c r o t e x t u r e o f
t h i s r o c k i s c h a r a c t e r i z e d by t r e m o l i t e and c u m m i n g t o n i t e g r a i n s t h a t
I------- 1
1 meter
F ig u re 9.
C a t a c l a s t i c pods i n h i g h l y w e a t h e r e d s h e a r z o n e .
o c c u r i n b o t h b l o c k fo rm and a s b u n d l e s o f s h e a r e d g r a i n s s u r r o u n d i n g
those blocks.
been broken.
B o t h a m p h i b o l e s e x h i b i t u n d u l o s e e x t i n c t i o n and ha v e
E x te n siv e a l t e r a t i o n of th e s e am phiboles is p re s e n t.
30
Subhedral
garnets
occur
as
layers
and
ty p ic a ll y coated w ith iro n - tita n iu m
grain
boundaries.
cracked,
This
rock
has
as
clu sters.
G arnets
are
o x i d e p h a s e s i n c r a c k s and a t
been
in ten sely
s tr o n g ly undulose g ra in s p re s e n t in t h i s
deform ed.
The
rock record d u c ti le
e f f e c t s t h a t were su b seq u e n tly s u b je c te d to b r i t t l e d efo rm atio n .
Another unique occu rren ce of a m p h ib o lite
m eter-scale
lens-shaped
L e v e r i c h Cree k o u t c r o p
actin o litite
(L—I ;
Figure
10).
po d
facies
that
m etabasite is
occurs
w ith in
a
a
Q uartzofeldspathic gneisses
1 meter
F i g u r e 10.
L e n s - s h a p e d a c t i n o l i t i t e pod .
wrap around t h i s
pod.
The pod i s h i g h l y w e a t h e r e d ,
m easurable s t r u c t u r a l data.
It
is
o b l i t e r a t i n g any
t h e r e f o r e not c l e a r what t h i s
pod
31
represents.
The pod i s e s e n t i a l l y a m o n o m i n e r a l i c a c t i n o l i t i t e w i t h a
m ajo r amount of i r o n - t i t a n i u m
b io tite
and r e t r o g r e s s i v e
( d e f in e d by Spry,
oxide phases
chlorite.
A relict
and t r a c e
decussate
am ounts of
m icrotexture
1969 a s i n t e r l o c k i n g , r a n d o m l y o r i e n t e d p r i s m a t i c
c r y s t a l s ) c h a r a c t e r i z e s t h i s rock,
although i t has been r e c r y s t a l l i z e d
to th e p o in t of appearing n e a rly g r a n o b la s tic .
No e v i d e n c e o f s t r a i n
i s found w i t h i n t h i s ro c k .
T ra n s itio n a l G ra n u lite Facies M etabasites
M afic ro ck s of th e t r a n s i t i o n a l g r a n u l i t e
facies
are lo c a lly
p r e s e n t and a r e c h a r a c t e r i z e d b y t h e d o m i n a n t a s s e m b l a g e h b l + p l a g +
diop
+ /-
sal
exposure is
+ gt
and
tex tu res
suggestive
a m e t e r - s c a l e l e n s - s h a p e d pod.
of
th at
grade.
One
The o t h e r o c c u r s a s a
m e te r-s c a le outcrop.
M ineralogy
M i n e r a l a s s e m b l a g e s a r e s u m m a r i z e d i n T a b l e 3.
of each th in
section
include
i r o n —t i t a n i u m
include
sericite,
are lis te d
oxides,
chlorite,
are d io p sid ic to s a l i t i c .
i n A p p e n d i x D.
sphene,
and z i r c o n .
and e p i d o t e .
M ineral contents
A ccessory phases
R etrograde phases
Clinopyroxene
com positions
R e t r o g r a d e p a t c h e s o f common h o r n b l e n d e
o c c u r on c l i n o p y r o x e n e g r a i n s .
A ll o th e r m in e ra ls found w ith in th e
t r a n s i t i o n a l g r a n u l i t e s have been p r e v i o u s l y d e s c r i b e d i n t h e q u a rtz o —
feldspathic
gneiss
section.
32
T a b l e 3.
T r a n s i t i o n a l g r a n u l i t e f a c i e s m e ta b a s ite assem blages.
hbl + p lag + q tz + g t + diop
hbl + plag + qtz + b t + s a l
hbl + plag + gt + s a l
hbl + p lag + q tz + diop
hbl + plag + gt + s a l
Textures
T ransitional
granulite
facies
and l e s s ) t o medium (2-3 mm).
displaying
penetrative
grain
sizes
range from f i n e
Textures a re v a ria b le .
deform ational fea tu re s
(.5mm
Those t e x t u r e s
on a m i c r o s c o p i c s c a l e
a re c h a r a c te r iz e d by nem ato b l a s t ic hornblende w ith i n t e r s t i t i a l g ra in s
of w e l l- r e c r y s ta ll i z e d
p l a g i o c l a s e and q u a r t z .
One s u c h r o c k o c c u r s
a s a m e t e r - s c a l e l e n s - s h a p e d pod w i t h i n t h e L e v e r i c h C r e e k o u t c r o p (L1; F i g u r e 1 1 ) .
The o n l y e v i d e n c e o f s t r a i n i n t h i s r o c k i s t h a t some
b io tite
grains
places.
Very
grains.
It
represents
ex h ib it
slig h t
is
not
unequal b ire frin g e n c e
to
clear
as th e r e i s
w ith
gn eisses
that
the
from
occurs
ob serv atio n s
what
(Figure
surrounding
surround th is
q u a rtz o fe ld s p a thie
pod e x h i b i t
planar
quartz
th is
gneisses.
fo liatio n ,
p od
The
though
i n t r a f o l i a l is o c lin a l folds are pre­
pod d e s c r i b e d i n t h e a m p h i b o l i t e f a c i e s
10).
in
evidence f o r d e te rm in in g w hether
T h i s pod o c c u r s o n l y "20 m e t e r s away fro m t h e
actin o litite
tio n
ex tin ctio n
in
T h is pod i s c o n f o r m a b l e and i s i n s h a r p
several local cen tim eter-scale
sent.
field
insufficient
o r n o t t h e pod i s f o l d e d .
co n tact
no u n d u l o s e
and p le o c h r o is m
Both of t h e s e pods l i e
m eter-scale
m etabasite sec­
in th e same o r i e n t a t i o n
33
qf gneiss
soil and float
1 meter
F i g u r e 11.
Lens-shaped t r a n s i t i o n a l g r a n u l i t e m e ta b a s ite .
w i t h i n t h e o u t c r o p and a r e e s s e n t i a l l y
granoblastic
w hile th e ir sur­
roun d ing g n e is s e s have r e t a i n e d m i c r o t e x t u r a l e v id e n c e of in te n s e
deform ation.
It
i s p o s s i b l e t h a t t h e pod s w e r e d e f o r m e d a t t h e same
t i m e a s a l l o t h e r l i t h o l o g i e s e x p o s ed a t t h i s o u t c r o p .
t h e pods so w e l l r e c r y s t a l l i z e d ?
Bo th pods a r e m a f i c .
I f s o , why a r e
I t is lik ely
t h a t t h e e q u i l i b r a t i o n r a t e s o f t h e m e t a b a s i t e pod s may ha v e d i f f e r e d
from t h e q u a r t z o f e l d s p a t h ie g n e i s s e s due to t h e i r c o n t r a s t i n g b u lk
com positions.
The g r a n o b l a s t i c t e x t u r e r e t a i n e d w i t h i n t h e m a f i c
t r a n s i t i o n a l g r a n u l i t e u n i t may r e p r e s e n t l o c a l c o n d i t i o n s w h e r e PH20
34
was
< PTotal during
the
later
am phibolite
facies
metamorphic event.
T h i s may h a v e e n a b l e d t h e t r a n s i t i o n a l g r a n u l i t e t o p e r s i s t , s e a l e d
fro m t h e e f f e c t s o f an a m p h i b o l i t e o v e r p r i n t .
nation fo r th is c o n trast is
em placed.
that
Another p o s s ib l e ex p la­
t h e pod s may h a v e b e e n t e c t o n i c a l l y
T h e r e i s no d i r e c t e v i d e n c e o f s h e a r i n g a t t h e c o n t a c t s
b e t w e e n t h e pod s and t h e g n e i s s e s t h a t e n c l o s e th em .
however,
It
is possible,
t h a t any e v id e n c e o f s h e a r i n g has s i n c e b e e n o b l i t e r a t e d
through r e c r y s t a l l i z a t i o n .
G ran o b lastic
textures
are r e p r e s e n ta tiv e of th o se rocks th a t
experienced com plete r e c r y s t a l l i z a t i o n .
A unique g r a n o b la s tic t e x t u r e
i s f o u n d i n a c o r o n a t e x t u r e (S p ry , 1969) m e t a b a s i t e t h a t o c c u r s i n
the
Sour dou gh C re ek d r a i n a g e a r e a .
ize d by a s t a t i c
is
m icroscopically
character­
overgrow th of w e l l r e c r y s t a l l i z e d g r a n o b la s tic horn­
b le n d e rimming s a l i t e n u c l e i .
tic
It
T h e s e n u c l e i a r e commonly p o i k i l o b l a s -
w ith p lagioclase inclusions.
Salite
grains
a r e c h a r a c t e r i z e d by
a n a b u n d a n c e o f h o r n b l e n d e o c c u r r i n g i n t h e f o rm o f p a t c h e s o r a l o n g
c l e a v a g e s and f r a c t u r e s .
and s a l i t e
n u clei.
Garnet rim s a re p re s e n t betw een p la g io c la s e
Some s m a l l n u c l e i o f g r a n o b l a s t i c
hornblende
c o n t a i n g a r n e t and i r o n - t i t a n i u m o x i d e s i n t h e i r c e n t e r s .
l i n e a t i o n o f some c o r o n a r i m s and i r o n - t i t a n i u m
observed,
hinting
r o c k may r e p r e s e n t
A rough
o x i d e g r a i n s was
a t a o nc e p r e s e n t f o l i a t i o n .
The t e x t u r e o f t h i s
tran sitio n al
c o n d i t i o n s b a s e d on
granulite
facies
t h e o b s e r v a t i o n t h a t s a l i t e g r a i n s show e v i d e n c e o f r e p l a c e m e n t by and
r e a c tio n to hornblende.
this
assem blage.
F i g u r e 12 i l l u s t r a t e s t h e ACF d i a g r a m f o r
35
A
F i g u r e 12.
ACF d i a g r a m f o r c o r o n a t e x t u r e m e t a b a s i t e .
M an na a n d Sen ( 1 9 7 4 ) h a v e m ade t h e o b s e r v a t i o n t h a t
iso b aric
c o o lin g of a g ab b ro ic m e lt has produced c o ro n a l t e x t u r e s
in m afic
granulite
gneisses
fro m
Saltora,
India.
J a m e s and Hedge
(1980) hav e
r e p o r t e d t h e i n t r u s i o n o f m a f ic m e l t s j u s t b e f o r e and d u r i n g a h ig h
g r a d e m e t a m o r p h i c e v e n t i n t h e Ruby R a n g e .
I t is p o stu lated th at
m a f i c g r a n u l i t e g n e i s s e s i n t h e K e l l y a r e a o f t h e Ruby Range may hav e
o r i g i n a t e d as a g a b b r o ic m e lt i n t r u d i n g deep in a g e o s y n c l i n a l p i l e
j u s t b e f o r e o r d u r in g m etam orphism (K a ra se v ic h , e t a l ,
m o d e l may b e r e a l i s t i c
study area.
1981).
T his
fo r th e corona te x tu r e rock observed in the
The l a c k o f an o b s e r v a b l e c r o s s - c u t t i n g
relationship
of
36
t h e c o r o n a t e x t u r e m e t a b a s i t e w i t h i n t h e s t u d y a r e a makes an i g n e o u s
o r ig i n uncertain.
P rotolith
T hin-layered m etab asite u n its
q u a rtz o feld sp a th ic
o u tlin ed
gn eisses
o c c u r as continuous u n i t s w ith in
in th e study area.
O rv ille
(1969) h as
t h r e e m e c h a n i s m s b y w h i c h t h i n —l a y e r e d m e t a b a s i t e s c a n b e
produced:
1.
M eta-igneous:
recry stallizatio n
as i n t r u s i v e s i l l s ,
2.
M etasedim entary:
dikes,
of b asic
igneous
e x tru s iv e flow s,
rocks
such
or tu ffs;
r e c r y s t a l l i z a t i o n of m arl or c a rb o n a te ­
bearing shale;
3.
M etaso m atic:
recry stallizatio n
of
some p a r e n t
m aterial
com bined w i t h a d d i t i o n a n d /o r s u b t r a c t i o n o f s i g n i f i c a n t
amounts of n o n v o l a t i l e c o n s t i t u e n t s .
Due t o
the
lack
of
cro ss-cu ttin g
relatio n sh ip s
and w i t h o u t
g e o c h e m i c a l a n a l y s e s , one c a n o n l y s p e c u l a t e a b o u t t h e o r i g i n o f s t u d y
area m etabasites.
pred o m in an tly
E v i d e n c e f ro m s u r r o u n d i n g r a n g e s i s s u g g e s t i v e o f a
igneous
o rig in
M ontana A rch ean e x p o s u r e s .
for
man y a m p h i b o l i t e s
in
southw est
Whole r o c k c h e m i c a l and N i g g l i v a l u e s
d e t e r m i n e d f o r e i g h t a m p h i b o l i t e s i n t h e C opper M o u n ta i n and K e l l y
a r e a o f t h e Ruby Range show t h a t m a s s i v e , b a n d e d ,
and s a l t and p e p p e r
v a r i e t i e s e x h ib i t i d e n t i c a l bulk chem ical com positions which a re s im i­
l a r to a m p h ib o lite s
in
t h e M adison
(S p e n ce r and Kozak,
1 9 7 5 ) , a n d B e a r t o o t h R a n g e (Van d eK am p,
T h e ir whole rock co m p o sitio n s s t r o n g l y
(F oster,
1962),
S panish Peaks
resem ble t h o e l i i t i c
1969).
basalts.
37
In a d d itio n ,
t h e i r N i g g l i Ca/Mg and A l - A l k /Ca r a t i o s
(Leake,
1964) a r e
c o m p a t i b l e w i t h i g n e o u s t r e n d s and a r e o b l i q u e t o t r e n d s e x p e c t e d f o r
calcareous shales.
are
displayed
Ken S a l t
C ross-cutting r e l a ti o n s h ip s
w ith in m etabasites
i n t h e s o u t h e r n Tob ac co Root Range.
(perso n al communication) has i d e n t i f i e d
g a b b r o and d i a b a s e
textures
a r e a o f t h e M a d is on Range.
and i g n e o u s t e x t u r e s
w ithin
m etabasites
cross-cutting
of th e
relict
S p a n i s h Pea ks
Evidence f o r th e a m p h ib o lite u n i t s o ccur­
rin g w ith in sedim entary u n its l i e s
in the observations th a t q u a rtz ite
i n t e r b e d s h a v e b e e n o b s e r v e d i n some o u t c r o p s and c o n g l o m e r a t i c u n i t s
have been re p o rte d
1980).
w ith in
am p h ib o lites
i n t h e Ruby R a n g e ( S m i t h ,
38
MYLONITES
M ylonites
are
recognized as p ro d u cts of s t r a i n
softening
repre­
s e n t a t i v e o f an a c c o m m o d a t i o n o f an i m p o s e d s t r a i n r a t e w i t h i n d u c t i l e
sh ear zones
(W hite e t a l ,
1980).
The l o c a l i z a t i o n
of high s t r a i n
r a t e s commonly o c c u r s w i t h i n a p p r o x i m a t e l y p l a n a r z o n e s known a s s h e a r
b elts
(Ramsay and G raham , 1970).
V arying d e g re e s of m y l o n i t i z a t i o n
a re r e f l e c t e d in study a re a rock f a b r i c s .
zone w i t h i n
the H y alite
presence of a lo c a liz e d
Creek o u tc r o p
s h e a r z o ne .
A m eter-scale ultam ylonite
(H-I) b e s t e x e m p l i f i e s t h e
T h i s u l t r a m y l o n i t e zon e i s
com­
p o s e d o f v e r y f i n e - g r a i n e d ( < <.5mm) q u a r t z - r i c h r o c k s w i t h g a r n e t ,
plagioclase,
tourm aline,
and c u m m i n g t o n i t e a s a c c e s s o r y p h a s e s .
of th e s e m in e ra ls e x h ib i t evidence of s t r a i n .
All
F o l i a t i o n i s d e fin e d by
a p re fe rre d o r ie n ta tio n of b i o t i t e
grains,
quartz
o f d u c t i l e y d e f o r m e d q u a r t z a ro u n d
ribbons,
porphyroblasts.
Garnets
and f l o w t e x t u r e s
( F i g u r e 13),
Quartz occurs as r i b b o n s and r e c r y s t a l l i z e d
ty p ic a lly contain
in th e rock.
ovoid g a r n e t s
inclusions
of a l l
G arnets, p la g io c la s e ,
grains.
the o th e r m inerals
fo u n d
t o u r m a l i n e , and c u m m in g to n ite
g r a i n s o c c u r as p o r p h y r o b l a s t s and r e p r e s e n t b r i t t l e m i n e r a l s i n a
d u c tile qu artzo se m atrix.
p lastic
deform ation,
M i t r a (1978).
(< <.5mm) and i s
T h e s e m i n e r a l s do n o t s h o w e v i d e n c e o f
t h o u g h some g r a i n s
are
c r a c k e d a s d e s c r i b e d by
B i o t i t e o c c u rs as v e ry f i n e l y - r e c r y s t a l l i z e d g r a i n s
m icrofolded
in places
(Figure
13).
Extensive
t a l l i z a t i o n o f q u a r t z and b i o t i t e o c c u r s i n t h e m y l o n i t e s .
recrys­
39
0.5 mm
F i g u r e 13.
U ltram ylonite.
S k e t c h e d f ro m a m i c r o p h o t o g r a p h t a k e n i n
p lan e-p o larized lig h t.
G arnet p o r p h y r o b la s ts occur as
b r i t t l e m in e ra ls in a p red o m in an tly q u a rtz o s e d u c t i l e
m atrix.
Note m i c r o f o l d e d r e c r y s t a l l i z e d b i o t i t e .
M icrostructural c h a ra c te ris tic s
of p l a s t i c a l l y deformed m in e r a ls
in m y lo n ites y i e l d c lu e s as to the p h y s ic a l p a ra m ete rs of deform ation
(B oullier,
1980).
H y a l i t e Creek m y l o n i t e s
of c r y s t a l p l a s t i c i t y .
exhibit
several properties
Evidence of d i s l o c a t i o n g l i d e as a de fo rm atio n
m echanism was o b s e r v e d in t h e f o l l o w i n g fo rm s o f i n t r a c r y s t a l l i n e
strain:
u n d u l o s e e x t i n c t i o n , s l i p b a n d s , d e f o r m a t i o n b a n d s , and c r y s ­
tallographic preferred orientations.
observed
include
subgrains
Accompanying r e c o v e r y s t r u c t u r e s
and r e c r y s t a l l i z e d
g r a i n s along g r a i n
40
boundaries.
grains
D i s l o c a t i o n c r e e p comm only y i e l d s
(T ullis
et al,
1982).
flatten ed
Ovoid g a r n e t p o r p h y r o c l a s t s
o rig in al
w ithin
m y l o n i t e s a t t e s t t o f l a t t e n i n g and s e r v e a s s t r a i n i n d i c a t o r s
13; R o s s ,
1973).
the
(Figure
E lo n g ate a re a s of s m a ll s t r a i n - f r e e polygonal to
inequant g ra in s of q u artz w ith su tu red g ra in boundaries a lso a t t e s t to
a high r a te
1973).
of s tr a in
T u llis,
et al
and t o s y n t e c t o n i c
rec ry stallizatio n
(Ross,
(1973) h a v e i n d i c a t e d t h a t s m a l l s t r a i n - f r e e
poly g o n al g r a i n s around l a r g e r o r i g i n a l g r a i n s r e p r e s e n t a hig h temp­
erature
of r e c r y s ta ll i z a t io n
deform ation.
and a r e p r o b a b l y r e l a t e d
to p la s tic
These f e a t u r e s have been observed w i t h i n th e H y a lite
Creek m y l o n i t e s .
R ed u ctio n s in g r a i n s i z e have a ls o been o bserved.
R ecrys t a l I i z atio n -acco m o d ated d is lo c a tio n
creep under in c re a sin g
s t r a i n c o n d i t i o n s has been a t t r i b u t e d by s e v e r a l a u t h o r s t o be resp o n ­
s i b l e f o r t h e g r a i n s i z e r e d u c t i o n and s t r a i n s o f t e n i n g c o n d i t i o n s
t h a t l e a d t o t h e f o r m a t i o n o f many m y l o n i t e s and d u c t i l e s h e a r z o n e s
(e.g. M i t r a , 1978; B o u l l i e r , 1980; W h ite e t a l ,
Yund,
1985).
strain,
1980; and T u l l i s and
Many o f t h e c h a r a c t e r i s t i c s o f t h e m y l o n i t e s
very fin e grain siz e ,
(e.g. h i g h
m ixing of m in e ra l phases which p rev en t
g r a in grow th) a re s u g g e s tiv e of a b u lk of s u p e r - p l a s t i c b e h a v io r of
t h e r o c k s a s p r o p o s e d b y B o u l l i e r and Gueguen (1975).
W hite
(1979)
has
characterized
shear
zones
as
"exam ples
of
i nh om oge no us d e f o r m a t i o n a r i s i n g b e c a u s e t h e c o u n t r y r o c k i s i n c a p a b l e
of
acco m o d atin g
deform ation.
of
im posed
stra in
rate
by b u lk
inhomogenous
Large s t r a i n s c o n c e n tra te in th e s e zones because of
soften in g w ith in
in d icativ e
an
them ."
such
M i c r o s t u c t u r e s of study a re a m ylonites a re
a zone
of
strain
co n cen tratio n .
Study
area
41
m ylonite
assem blages
do
not
yield
metamorphism th ey formed under.
clues
as
to
what
grade
of
However, i t i s b e l i e v e d t h a t t h e y d i d
n o t f o rm u n d e r p e a k m e t a m o r p h i c c o n d i t i o n s a s t h e r o c k s h a v e n o t b e e n
ex ten siv ely recry stallized .
A u n ique t e x t u r e o bserved w i t h i n a m y lo n itic u n i t occurs as a
psuedotachyIy te
and
provides
ad d itio n al
evidence
for
shearing
p ro cesses in the study area.
The p s e u d o t a c h y I y t e o c c u r s a s a d a r k ,
m i c r o c r y s t a l l i n e m a trix band,
sandwiched between a q u a r t z o f e l d s p a t h ic
gneiss
th is
u n it.
C ontacts
w ith
u n i t a re sh a rp e x c e p t where th e
p s e u d o t a c h y I y t e l o c a l l y i n v a d e s t h e s u r r o u n d i n g g n e i s s ( F i g u r e 14).
Numerous r o u n d e d q u a r t z ,
c h l o r i t e - r i c h m atrix.
h av in g
undergone
hornblende,
and e p i d o t e g r a i n s l i e w i t h i n a
The p s e u d o t a c h y I y t e ba n d e x h i b i t s
d u ctile
d efo rm atio n
based
evidence of
on t h e
follow ing
observations:
1.
I n c lu s io n s in th e m a trix d is p la y undulose e x ti n c ti o n ;
2.
X e n o c r y s t s o f q u a r t z and f e l d s p a r a r e l e n t i c u l a r i n s h a pe ;
3.
M icrofolds a re p rese n t w ith in the m atrix;
4.
A strong
grains,
preferred
p arallel
o rien tatio n
to f o l i a t i o n ,
of
opaques
and
ch lo rite
occurs in th e surrounding
quartzofeldspathic g n e iss.
Several authors
and
1977;
and
W atts
(e.g. A l l e n ,
1979; F r a n c i s ,
and W illia m s ,
1979)
1 9 7 2 ; S i b s o n , 1975
have
suggested
th at
p s e u d o ta c h y ly t e bands d evelop by l o c a l m e l ti n g of ro ck i n resp o n se t o
f r i c t i o n a l h e a t g e n e r a t e d by s e i s m i c s l i p on a b r i t t l e
A decrease
in
tem p e ra tu re during
retrogression
is
shear fracture.
p r o b a b l y t h e mai n
reason f o r gradual s t r a i n hardening lea d in g to in c r e a s in g d i f f e r e n t i a l
42
0.5 mm
F i g u r e 14.
P seudotachylyte te x tu re .
Note s h a rp c o n t a c t b e tw e en
p s e u d o t a c h y l y t e and s u r r o u n d i n g q u a r t z o f e l d s p a t h i c g n e i s s .
s t r e s s e s and f i n a l l y t o t h e g e n e r a t i o n o f p s e u d o t a c h y l y t e s
1982).
(Passchier,
The m i n e r a l p a r a g e n e s e s i n s t u d y a r e a p s e u d o t a c h y l y t e s a r e
co n sisten t
w ith
transform ation
the
from
retrograde
am phibolite
assem b lag es
to
r e f l e c t ive
g ran u lite
facies
of
the
co nditions.
Deformed p s e u d o ta c h y ly t e bands a r e g e n e r a te d a t c r u s t a l l e v e l s in
betw een
the
zon e w h e r e d u c t i l e
where b r i t t l e
(P asschier,
fractu rin g
1982).
deform ation is
produces
d o m i n a n t and t h e zone
undeform ed
p seu d o tach y ly tes
43
In
tex tu res
summ ary,
the
in th e
study
presence
area
deform ation th a t a ffe c te d
is
reflectiv e
of
of
a ttest
the area.
c o n d itio n s
of
m y lo n itic
to
the
and
pseudotachylitic
in ten sity
and
sty le
of
Evidence of d u c t i l e d e fo rm atio n
high
m etam o rp h ic
grade.
The
l o c a l i z a t i o n of th e s e t e x t u r e s i s su g g e stiv e of th e p resen ce of form er
shear zones.
44
METAMORPHISM
B a s e m e n t r o c k s i n s o u t h w e s t M ontana u n d e r w e n t h i g h g r a d e r e g i o n a l
metamorphism.
The f o l l o w i n g o b s e r v a t i o n s o f t h e s e r o c k s a r e i n d i c a ­
t i v e of p ro g ra d e m etam orphic c o n d itio n s w hich s tr a d d le d th e upper
a m p h i b o li t e / l o w e r g r a n u l i t e grade boundary:
1.
E v i d e n c e o f t r a n s i t i o n b e t w e e n t h e two f a c i e s
is
exhibited
by c o r o n a t e x t u r e s i n some m e t a b a s i t e s ;
2.
G ranoblastic te x tu re s are p resent;
3.
Dark o l i v e - g r e e n h o r n b l e n d e and deep r e d p l e o c h r o i s m i n b i o tite
4.
occur;
P e rth itic kspar is p resent.
Figure
15 i l l u s t r a t e s
a petrogenetic
g rid c o n s tr a in in g tem pera­
t u r e and p r e s s u r e c o n d i t i o n s f o r s t u d y a r e a r o c k s .
The c o n d i t i o n s
of
t h e s e p a r a m e t e r s w e r e e v a l u a t e d u s i n g p u b l i s h e d e x p e r i m e n t a l and t h e o ­
r e t i c a l d a t a on p e r t i n e n t r e a c t i o n s c o m b i n e d w i t h g e o t h e r m o m e t r i c
s t u d i e s o f g a r n e t - b i o t i t e and g a m e t - c l i n o p y r o x e n e p a i r s .
E v a lu a tio n of m etamorphic c o n d it io n s i s d i f f i c u l t because of th e
p a r t i a l r e e q u i l i b r a t i o n o f r e l i c t a s s e m b l a g e s a s w e l l a s a. l a c k o f
lim itin g reactions.
The m e t a m o r p h i c c o n d i t i o n s o f Ml a r e c o n s t r a i n e d
by t h e p r e s e n c e o f s i l l i m a n i t e and e v i d e n c e o f p a r t i a l m e l t i n g i n t h e
form of m ig m a t i te s i n q u a r t z o f e l d s p a t h i c g n e i s s e s .
g arn e t-b io tite
tem peratures
of
and
g arn et-clin o p y ro x en e
6 8 0 ° - 7 20° (David Mogk1 p e r s o n a l
In a d d itio n ,
g eotherm om etry y i e l d
communication).
o b s e r v a t i o n s im ply p r e s s u r e s of be tw e en 5-7 k i l o b a r s
( F i g u r e 15).
These
The
45
pH 2 O 1 k b a r
■
F i g u r e 15.
T e m p e r a t u r e - p r e s s u r e d i a g r a m f o r m e t a m o r p h is m o f t h e s t u d y
area.
Ml r e f l e c t s t r a n s i t i o n a l g r a n u l i t e f a c i e s
c o n d i t i o n s . Arrow i l l u s t r a t e s t h a t o v e r p r i n t e d e p i d o t e am p h ib o lite
facies
assem b lag es
(M2) r e p r e s e n t
r e t r o g r e s s i o n from t r a n s i t i o n a l g r a n u l i t e f a c i e s
c o n d i t i o n s (M l).
E xcess q u a rtz is assum ed in a l l
r e a c tio n s . Solid l i n e s i n d i c a t e e x p e r i m e n t a l l y v e r i f i e d
reactio n s.
Dashed l i n e s i n d i c a t e e x t r a p o l a t e d l i n e s .
R e a c t i o n s shown a r e :
I) ky<-? a n d ^ s i l (Holdaway, 1971);
2) minimum m e l t i n g c u r v e f o r common g r a n i t e ( T u t t l e and
Bowen, 1958); and 3) muse + q t z 4^ k s p + H20 (Evans, 1965).
46
m e t a m o r p h i c c o n d i t i o n s o f M2 a r e b a s e d on t h e p r e s e n c e o f e p i d o t e and
the lack of p a r t i a l l y
m elted q u a rtz o f e ld s p a th ic g n e isse s.
e x h i b i t evidence of l a t e
1.
Most r o c k s
(p ost-M2) r e t r o g r a d e e f f e c t s b a s e d on:
The p r e s e n c e o f e x t e n s i v e c h l o r i t i z a t i o n
and p l a g i o c l a s e
seritizatio n ;
2.
The r e p l a c e m e n t o f p y r o x e n e b y a m p h i b o l e s ;
3.
The r e p l a c e m e n t o f common h o r n b l e n d e b y h a s t i n g s i t i c h o r n ­
b l e n d e and p l a g i o c l a s e b y e p i d o t e .
The c a u s e o f r e t r o g r e s s i o n
reflect
facies
eith er
a sep arate,
conditions
s t a g e s o f M2.
is
latest
uncertain.
R etrograde
facies
(M-3?) e v e n t u n d e r g r e e n s c h i s t
or retrograde processes
a s s o c i a t e d w i t h t h e waning
47
DEFORMATION
B a s e m e n t r o c k s i n s o u t h w e s t M on tan a ha v e b e e n i n t e n s e l y d e f o r m e d .
W i t h few e x c e p t i o n s , t h e r e g i o n a l s t r u c t u r a l g r a i n o f A r c h e a n r o c k s i n
s o u t h w e s t Montan a i s
to th e n o r th e a s t
c h a r a c t e r i z e d by f o ld axes t h a t g e n e r a ll y tre n d
(S p e n c e r and K ozak,
F o u n t a i n and D e s m a r a i s ,
1980).
1975; V i t a l i a n o ,
et al,
1979;
Throughout th e stu d y a r e a a s t r u c t u r a l
g r a i n i s e x p r e s s e d b y f o l i a t i o n t h a t p r e d o m i n a n t l y s t r i k e s N45E a n d
dips s te e p ly to the n o rth w est or so u th e a st.
M i n e r a l l i n e a t i o n s and
f o l d h i n g e l i n e s p r e d o m i n a n t l y t r e n d n o r t h e a s t o r s o u t h w e s t and p l u n g e
m oderately to s te e p ly
in both d ire c tio n s .
e a s t and t h e n o r t h w e s t .
Exposures in th e study a re a a r e l i m i t e d
t o h e a v y f o r e s t a t i o n and a t h i c k
stru ctu ral
features
Folds verge to the south­
so il
found th ro u g h o u t
m antle.
the
Figure
due
16 i l l u s t r a t e s
study area.
Representative
s t e r e o n e t s a r e shown i n F i g u r e s 17-19.
A ll fo ld s in th e study area
o c c u r on a c e n t i m e t e r t o m e t e r - s c a l e
and e x h i b i t a s i m i l a r s t y l e o f f o l d i n g .
Two f o l d t y p e s o c c u r and a r e
most e a s i l y r e c o g n iz e d w i t h i n w e l l - f o l i a t e d q u a r t z o f e l d s p a t h i c g n e i s ­
ses.
The e a r l i e s t r e c o g n i z e d p e r i o d o f d e f o r m a t i o n p r o d u c e d c e n t i ­
m eter to m e te r-s c a le p assiv e-flo w i s o c l i n a l fo ld s
are i n tr a f o l ia l
p arallel
to
folds
rock
( F i g u r e 20).
fo liatio n .
(F I) ,
some o f w h i c h
The a x i a l p l a n e o f t h e s e f o l d s
Some F l
is
fo ld s a re recum bent. Q uasi-
f l e x u r a l f o l d s w e r e a l s o p r o d u c e d d u r i n g F l and a r e r e p r e s e n t e d by
ptyg m atically
folded
leucosom es
and
disharm onic
folding
w ith in
Legend
-t"
foliation
4 /
44
trend and plunge
of Iineation
21
trend and plunge
of fold hinge line
(p a t te r n s indicate gene ra l
fold s h a p e s )
Figure
16.
1 mile
G e n e r a l i z e d s t r u c t u r e map f o r s t u d y a r e a .
( L e t t e r e d l o c a t i o n s e x p l a i n e d i n t e x t and
in ste r e o n e t c a p tio n s.
See a l s o Appendix A . )
49
H
a.
H y a l i t e Canyon (H-I)
N 52 E, 70 SE.
71 p o l e s .
C o n t o u r s , 1%, 3%, 20%
30%, p e r 1% a r e a .
b.
Hodgman Canyon (HD-I)
N 56 E, 50 SE.
50 p o l e s .
C o n t o u r s , 2%, 10%, 20%,
30%, p e r 1% a r e a .
c.
L e v e ric h Creek (L-I)
N 30 E, 17 SE.
140 p o l e s .
C o n t o u r s , 1%, 10%, 25%,
4%, p e r 1% a r e a .
d.
Sour do ug h Creek (S -13)
N 51 E, 84 NW,
N 69 E, 73 SE.
26 p o l e s .
C o n t o u r s , 1%, 5%, 10%,
15%, p e r 1% a r e a .
e.
Sourdough Cr e e k (S-12)
N 36 E, 82 NW,
N 36 E, 9 0 .
37 p o l e s .
C o n t o u r s , 1%, 5%, 15%,
25%, p e r 1% a r e a .
F i g u r e 17.
S te re o n e ts i l l u s t r a t i n g the g en eral s t r i k e of f o li a ti o n
from m a j o r o u t c r o p s w i t h i n t h e s t u d y a r e a .
50
N
N
b
a.
L e v e r i c h Creek ( L - I )
25. S 67 E.
32 p o i n t s .
C o n t o u r s . 1%. 3%, 10%,
20%, p e r 1% a r e a .
b.
N
N
d
C
c.
Sou rdough Cree k (S -12)
25. N 56 E.
18 p o i n t s .
C o n t o u r s , 1%, 5%, 15%,
20%, p e r 1% a r e a .
F i g u r e 18.
Sourdough Cr e e k (S-13)
40. N 63 E.
25 p o i n t s .
C o n t o u r s , 1%, 5%, 10%,
15%, p e r 1% a r e a .
d.
Sourdough Cr e e k (S-N)
22, N 39 E, 4 4 . S 41 W.
46 p o i n t s .
C o n t o u r s , 2%, 4%, 15%,
p e r 1% a r e a .
B i o t i t e s t r e a k and a m p h i b o l e l i n e a t i o n s t e r e o n e t s .
51
a.
Sour dough Creek (S -1 3 )
21, S 52 W. 44 p o i n t s .
C o n t o u r s , 2%, 5%, 10%
20% p e r 1% a r e a .
F i g u r e 19.
b.
Sourdough Creek ( S - 1 2 ) .
71 . N 29 E, 44 , S 60 W.
5 points.
Too few p o i n t s
to contour.
I s o c l i n a l and open f o l d h i n g e l i n e s t e r e o n e t s .
q u a rtz o feld sp ath ic
gneisses
(S-13; F i g u r e 21).
A second p e rio d of
s - 13>
d e fo r m a tio n produced f l e x u r a l - f l o w
F2 f o l d s
open f o l d s
coaxial w ith Fl
folds.
generally larg e r
(m eter-scale) than Fl folds.
(F2;
S - 14;
Figure
22),
a r e g e n e r a l l y n o t o v e r t u r n e d and a r e
The p r i n c i p a l d i r e c t i o n
of s t r a i n r e s p o n s i b l e f o r t h e d e f o r m a t i o n of t h e s e f o l d s must h av e
r e m a i n e d t h e same a s F2 f o l d s d e f o r m e d c o a x i a l l y w i t h F l f o l d s .
The
g e o c h ro n o lo g ic a l sequence of f o ld g e n e ra tio n s in th e study a re a is
b a s e d on t h e d e g r e e o f c l o s u r e on f o l d s
vation
that
F2 f o l d s
folded Fl f o l i a t i o n
(Davis,
19 84),
and t h e o b s e r ­
and c o m p o s i t i o n a l l a y e r i n g .
52
F i g u r e 20 .
I s o c l i n a l (Fl) i n t r a f o l i a l f o l d i n g o f l e u c o c r a t i c u n i t (L)
w i t h i n q u a r t z o f e l d s p a t h i e g n e i s s ( q f g n ) . L e n s c a p (C)
d i a m e t e r = 5 cm.
53
1 meter
F ig u re 21.
D ish a rm o n ic a lly fo ld e d
b o l i t e g n e isse s.
(F l) q u a r t z o f e l d s p a t h i c
and a m p h i­
54
1 meter
F ig u re 22.
O pen t o b r o a d f l e x u r a l - f l o w f o l d s ( F 2 ) .
D ashed
i n d i c a t e ap p ro x im ate p o s i t i o n s of f o ld h in g e l i n e s .
lin e s
55
B o th g e n e r a t i o n s o f f o l d s p r e s u m a b l y f o rm e d u n d e r h i g h g r a d e m e t a m o r p h ic c o n d itio n s.
A u n iq u e
fo ld
c e n tim e te r-sc a le ,
5b a s i n fo rm (S -1 4 ;
sty le
lie s
in a s e t o f open to b r o a d ly f o ld e d ,
q u a r t z o f e l d s p a t h i c s u p e r p o s e d f o l d s o f dom e a n d
F ig u re
23).
These f o ld s
appear to
represent
a
30 cm
F ig u re 23.
lo c a liz e d
a ffe c te d .
S u p e r p o s e d f o l d s o f dome and b a s i n fo rm .
t r e n d s i n d i c a t e d on p h o t o .
phenom enon
as
im m e d ia te ly
a d ja c e n t
The dome and b a s i n s u p e r p o s e d f o l d s
F o ld h in g e l i n e
fo ld s
e x h ib its
are
not
so
tw o d i f f e r e n t
f o l d h i n g e l i n e o r i e n t a t i o n s : 2 5 , d u e s o u t h ( f o l d s e t A, F i g u r e 2 3 ) ,
and 24,
S73W ( f o l d s e t B, F i g u r e 2 3 ) .
g en eral o r ie n ta tio n
e n t i r e o u tcro p .
The l a t t e r l i e s
as th e d o m in a n t f o l d h in g e l i n e
i n t h e sam e
tre n d
fo r th e
A g e o m e tric a n a ly s is o f rock f a b r ic to d e te rm in e th e
56
r e l a t i v e tim in g am ongst th e su p erp o sed f o ld s e ts i s n o t p o s s ib le as
t h e s t r u c t u r e d o es n o t c o n t a i n any l i n e a r m i n e r a l s .
Two r e a l i s t i c
p o s s i b l i t i e s w ith r e s p e c t to th e r e l a t i v e tim in g of f o ld fo rm a tio n a re
as fo llo w s.
The s u p e r p o s e d f o l d s c o u l d h a v e f o rm e d c o n t e m p o r a n e o u s l y
as a r e s u l t o f a x i a l l y sy m m e tric s h o r te n in g .
I f t h e tw o f o l d s e t s
f o rm e d a t d i f f e r e n t t i m e s , i t i s b e l i e v e d t h a t f o l d s e t B w o u ld r e p r e ­
s e n t t h e y o u n g e s t s e t o f f o l d s a s t h e y a r e m ore c o h e r e n t and p r o m i n e n t
t h a n f o l d s e t A.
The p r e f e r r e d i n t e r p r e t a t i o n i s t h e f o r m e r .
The
p r e s e n c e o f tw o f o l d h i n g e l i n e o r i e n t a t i o n s w i t h i n t h e dome and b a s i n
s t r u c t u r e i s n o t c o n s i s t e n t w i t h t h e s i n g l e d o m in a n t f o l d h i n g e l i n e
t r e n d fo u n d w i t h i n t h e s t u d y a r e a (~N45E, F i g u r e 16).
I t is th erefo re
n o t r e a l i s t i c t o c a l l u pon tw o s e p a r a t e n o n - c o a x i a l f o l d e v e n t s f o r
th e g e n e ra tio n o f superposed fo ld s .
One s t r u c t u r a l a n o m a ly e x i s t s w i t h i n t h e L e v e r i c h C reek o u t c r o p
(L -I).
L i n e a t i o n t r e n d s p lu n g e s o u t h e a s t (F ig u re 1 8a). T h is i s n o t
c o n s i s t e n t w i t h t h e p r e d o m i n a n t n o r t h e a s t t r e n d f o r f o l i a t i o n and f o l d
h in g e l i n e s
th ro u g h o u t th e s tu d y a re a .
u n d e te rm in a b le ,
1.
A lthough t h e a c t u a l c a u se i s
some p l a u s i b l e r e a s o n s f o r t h i s a n o m a ly a r e :
The l i n e a t i o n
rep resen ts
a tre n d
p e rp e n d icu la r to
th e h in g e
l i n e s of s o u th e a s t v e rg in g fo ld s in th e stu d y a re a ;
2.
The l i n e a t i o n
rep re se n ts
a
lo c a liz e d
phenom enon
due
to
r o t a t i o n o f a b lo c k a lo n g s h e a r z o n e s;
3.
L o c a l i z e d s t r a i n c o n d i t i o n s d i f f e r e d fro m t h o s e t h a t im p o s e d
th e predo m in an t n o r t h e a s t t r e n d .
57
CORRELATION OF DEFORMATION AND METAMORPHISM
B a se d on t h e p r e s e n c e
g ra n u lite
a sse m b la g e s,
it
of g ra n o b la stic
is b e lie v e d
te x tu re s
th a t
th e
and t r a n s i t i o n a l
e n tire
s tu d y a re a
i n i t i a l l y e x p e r i e n c e d t r a n s i t i o n a l g r a n u l i t e f a c i e s m e ta m o r p h is m (Ml).
M ig m a ti z a t i o n and t h e r e g i o n a l f o l i a t i o n
th e se
c o n d itio n s.
Iso c lin a l
fo ld s
th a t
(S I) w e r e p r o d u c e d u n d e r
are a x ia l
p la n a r to
f o l i a t i o n a r e a l s o c o n t e m p o r a n e o u s w i t h Ml c o n d i t i o n s .
th is
A d d itio n a l
e v i d e n c e f o r a t r a n s i t i o n a l g r a n u l i t e f a c i e s e v e n t com es fro m g e o t h e r ­
m o m e tric s t u d i e s .
D a v id Mogk ( p e r s o n a l c o m m u n ic a t io n ) h a s fo u n d t h a t
g a r n e t - b i o t i t e t e m p e r a t u r e s i n q u a r t z o f e l d s p a t h i c g n e i s s e s and g a m e t c lin o p y ro x en e te m p e ra tu re s
in th e m e ta b a site s of
l i t e g rad e y i e l d te m p e ra tu re s o f 680°-720°.
b e tw e e n 5-7 k i l o b a r s
tra n s itio n a l
granu­
P r e s s u r e s p ro b a b ly ranged
( F i g u r e 15).
B a s e d on t h e p r e d o m i n a n c e o f e p i d o t e - a m p h i b o l i t e f a c i e s a s s e m ­
b la g e s , th e p rese n c e of corona t e x t u r e s
p a tc h e s
on h o r n b l e n d e g r a i n s ,
in m e ta b a s ite s ,
h a stin g site
and t h e o b s e r v a t i o n t h a t no new s t r u c ­
t u r a l e le m e n ts have been i d e n t i f i e d w ith in e p id o te -a m p h ib o lite f a c ie s
rocks,
it
i s b e lie v e d t h a t e p id o te -a m p h ib o lite f a c ie s c o n d itio n s
w e r e o v e r p r i n t e d upon t r a n s i t i o n a l g r a n u l i t e f a c i e s r o c k s
se n tin g
a c o o l- d o w n o f t h e h i g h e r g r a d e "event (Ml).
(M2)
(Ml), r e p r e ­
D u c t il e deform a­
t i o n w as c o n te m p o r a n e o u s w i t h e p i d o t e - a m p h i b o l i t e f a c i e s
c o n d itio n s
(M2) a s m y l o n i t e s i n t h e s t u d y a r e a do n o t e x h i b i t a f u l l r a n g e o f
r e c r y s t a l l i z a t i o n and r e c o v e r y s t r u c t u r e s a s w o u ld b e e x p e c t e d i f t h e y
58
ha d b e e n p r o d u c e d u n d e r t h e e a r l i e r p e a k m e t a m o r p h ic c o n d i t i o n s
tra n sitio n a l
g ra n u lite
As d i s c u s s e d
(i.e .
facies).
i n t h e m e ta m o r p h is m s e c t i o n o f t h i s
th e sis,
g reen-
s c h i s t f a c i e s a s s e m b l a g e s o v e r p r i n t e d upon e p i d o t e —a m p h i b o l i t e f a c i e s
a s s e m b l a g e s r e p r e s e n t e i t h e r a g r e e n s c h i s t m e t a m o r p h ic e v e n t (M—3?) o r
retro g ra d e
e ffe c ts
a s s o c i a t e d w i t h t h e w an in g s t a g e s o f e p i d o t e -
a m p h i b o l i t e f a c i e s m e ta m o r p h is m (M2).
A s m a l l num ber o f ro c k s w i t h i n t h e s tu d y a r e a e x h i b i t e v id e n c e o f
b rittle
f a i l u r e on a l o c a l s c a l e .
a m p h ib o lite f a c ie s
As t h e s e r o c k s c o n t a i n e p i d o t e -
a s s e m b la g e s and e x h i b i t e v id e n c e o f e x t e n s i v e
r e t r o g r e s s i o n , c o n d i t i o n s c o n d u c iv e to b r i t t l e b e h a v io r m ust have
o c c u r r e d a f t e r M2.
I t a p p e a rs t h a t F l f o ld s w ere produced d u rin g t r a n s i t i o n a l gran u ­
lite
f a c i e s c o n d i t i o n s and t h a t b r o a d open c o a x i a l f o l d s r e f l e c t a
s e c o n d f o l d e v e n t (F2) a s t h e y f o l d t h e r e g i o n a l f o l i a t i o n ( S I ) .
i s u n c e r t a i n a s t o w h e t h e r F2 f o l d s w e r e p r o d u c e d a s p a r t
It
o f one
c o n t i n u i n g m e t a m o r p h ic c y c l e d u r i n g t h e w a n in g s t a g e s o f t r a n s i t i o n a l
g r a n u l i t e f a c i e s c o n d i t i o n s o r l a t e r a s a s e p a r a t e m e t a m o r p h ic c y c l e ,
p erh ap s under e p id o te -a m p h ib o lite c o n d itio n s .
research ers
(e.g . S p e n c e r and K o zak ,
F o u n t a i n and D e s m a r a i s ,
1980;
M u e lle r,
A lth o u g h num erous
1975; V i t a l i a n o ,
e t a l,
et a l,
1982) h a v e e s t a b l i s h e d
t h a t i s o c l i n a l f o l d s w e r e p r o d u c e d b e f o r e l a r g e op en f o l d s
w e s t M o n ta n a ,
1979;
in so u th ­
t h e s e tw o A rc h e a n f o l d i n g e v e n t s h a v e n o t b e e n a s s i g n e d
u n e q u iv o c a l ag es w i t h r e s p e c t t o a v a i l a b l e age d a te s .
S tu d y a r e a r o c k s p r o v i d e c l u e s t h a t c o n t r i b u t e t o a n i n t e r p r e t a ­
t i o n o f t h e r e g i o n a l A rchean m e ta m o r p h ic and d e fo r m a t i o n a l h i s t o r y .
59
The b e s t r e c o n s t r u c t i o n o f m e t a m o r p h ic and d e f o r m a t i o n a l e v e n t s t h a t
can be d is c e rn e d
fro m an i n t e g r a t i o n
o f p e t r o g r a p h i c and s t r u c t u r a l
o b s e r v a t i o n s w i t h i n t h e s t u d y a r e a and c o r r o b o r a t i v e e v id e n c e from
s u r r o u n d i n g r a n g e s i s p r e s e n t e d i n T a b l e 4.
T a b le .4.
I n t e r p r e t e d g e o c h r o n o l o g y o f m e ta m o r p h ic and d e f o m a t i o n a l e v e n t s
a f f e c t i n g b a s e m e n t l i t h o l o g i e s i n t h e n o r t h e r n G a l l a t i n R ange.
EVENT
EVIDENCE
T r a n s i t i o n a l g r a n u l i t e f a c i e s m etam orphism (M l),
m igm ati z t i o n , and i s o c l i n a l f o l d i n g ( F l ) .
P re se n c e o f corona t e x t u r e e x h ib i ti n g t r a n s i t i o n
fro m g r a n u l i t e t o u p p e r a m p h i b o l i t e c o n d i t i o n s .
T ig h tn e s s o f f o l d s i s i n d i c a t i v e o f an e a r l i e s t
fo ld e v e n t.
Upper a m p h ib o lite f a c i e s o v e r p r i n t
o p e n f o l d i n g ( F 2 ) , and d u c t i l e
m y lo n itiz a tio n .
U p p e r a m p h i b o l i t e m i n e r a l a s s e m b l a g e s . Openness
o f f o ld s i n d i c a t e s l a t e r s ta g e o f f o ld in g th an
(F I).
(M2),
G r e e n s c h i s t m etam orphism (M3?) o r r e t r o g r e s s i o n
fro m a m p h i b o l i t e f a c i e s c o n d i t i o n s .
G r e e n s c h i s t f a c i e s m i n e r a l a s s e m b la g e s r e p l a c i n g
a m p h ib o lite f a c ie s m in e ra ls .
B rittle fa ilu re .
C a t a c l a s t i c t e x t u r e s in a m p h ib o lite f a c i e s ro c k s .
61
TECTONIC MODEL
O b serv atio n s
R ange
can
be
te c to n ic s.
made o f A rc h e a n e x p o s u r e s i n t h e n o r t h e r n G a l l a t i n
used
to
A rch ean
g re e n s to n e -g ra n ite
B r id g w a te r , 1971;
ad d ress
th e
te rra n e s
s u b je c t
have
o fte n
or g r a n u lite -g n e is s
W in d le y , 1981).
of
re g io n a l
been
A rchean
su b d iv id e d
te rra n e s
in to
(W in d ley
and
Rocks r e p r e s e n t e d i n s o u th w e s t
M o ntana A r c h e a n e x p o s u r e s a r e c l e a r l y o f t h e l a t t e r c a t e g o r y , b a s e d on
th e p red o m in an c e of h ig h -g ra d e a s se m b la g e s .
T h e N o r t h Snowy B l o c k
m o b ile b e l t
in
d e fin e s
b e t w e e n tw o
f u n d a m e n ta lly d i s t i n c t A rchean t e r r a i n s
th e
B e a rto o th
Range l o c a l l y
th e b o u n d ary
in
th e n o rth e rn
Wyoming P r o v i n c e ; p r e d o m i n a n t l y c a l c - a l k a l i n e g r a n i t o i d s
east
and p r e d o m i n a n t l y m e t a s u p r a c r u s t a l r o c k s l i e
p re s e n c e of a m ajo r d i s c o n t i n u i t y
of la rg e -s c a le
in te c to n ic
tra n sc u rre n t fa u ltin g
sty le
to
lie
to th e
th e w est.
The
an d t h e p r e s e n c e
i n t h e N o r t h Snowy B lo c k m o b i l e
b e l t r e q u i r e t h a t t h e t e c t o n i c e v o l u t i o n o f A rc h e a n r o c k s o f t h e s t u d y
a r e a and a d j a c e n t r a n g e s t o t h e w e s t b e c o n s i d e r e d
se p a ra te ly
(Mogk,
e t a l, in rev ie w ).
The a b s e n c e o f d e t a i l e d g e o c h r o n o l o g i c and g e o c h e m i c a l d a t a f o r
t h e s t u d y a r e a a n d a d j a c e n t A r c h e a n e x p o s u r e s t o t h e w e s t m ake a n
in te rp re ta tio n
an y t e c t o n i c
of th e
te c to n ic
e n v iro n m en t v e ry d i f f i c u l t .
H ow ever,
m odel d e v e l o p e d f o r A r c h e a n r o c k s o f t h e s t u d y a r e a and
a d j a c e n t e x p o s u r e s t o t h e w e s t m u s t a c co m m o d a te t h e f o l l o w i n g o b s e r v a ­
tio n s ;
62
1.
Q u a r t z o f e l d s p a t h i c g n e i s s e s i n t h e s t u d y a r e a an d i n a d j a c e n t
r a n g e s r e p r e s e n t m e ta m o r p h o s e d q u a r t z - r i c h a n d im m a t u r e c l a s ­
tic
m e ta sed im e n ta ry
ro ck s
and a s su ch r e q u i r e
a silic ic
source.
The p r e s e n c e o f c a r b o n a t e s and q u a r t z i t e s
in ranges
w est
th e
p la tfo rm
of
stu d y a re a
is
a s s o c ia tio n s in th a t area.
su g g e stiv e
of s ta b le
I t h as been s u g g e s te d t h a t m eta­
s e d i m e n t a r y r o c k s i n t h e B l a c k t a i l Range w e s t o f t h e s tu d y
a r-e a may r e p r e s e n t t h e w e s t e r n e d g e o f a b a s i n p r o p o s e d b y
V ita lia n o ,
et al
(1979)
( C l a r k a n d M ogks
1985).
M arb le­
b e a r i n g s e q u e n c e s su c h a s t h o s e o f t h e T obacco Root Range
(V ita lia n o ,
et a l,
1979) r e p r e s e n t t h e b a s i n ' s c e n t e r and t h e
m a r b l e - d e f i c i e n t s e q u e n c e s o f t h e n o r t h e r n G a l l a t i n Range
rep resen ts
2.
t h e b a s i n 's e a s t e r n m arg in .
A deep c r u s t a l l e v e l i s
tio n a l
g ra n u lite
fa c ie s
1981; H en ry , e t a l ,
in d ic a te d by th e p re s e n c e of t r a n s i ­
a sse m b la g e s
( P e r k i n s and N e w to n ,
1982) and a s s o c i a t e d m i g m a t i t e s .
Tec­
t o n i c t h i c k e n i n g i s c o m p a t i b l e w i t h t h e p r e s s u r e and t e m p e r a ­
tu r e c o n d itio n s of th e s e rocks.
3.
L o c a liz e d
myl o n i t i c
fab rics
re fle c t
th e presence of d u c tile
shear zones.
4.
L a r g e - s c a l e i s o c l i n a l f o l d s an d n a p p e s ( d e f i n e d a s s h e e t l i k e ,
a l l o c h t h o n o u s r o c k u n i t s w h i c h h a v e b e e n moved on a p red o m ­
i n a n t l y h o r i z o n t a l s u r f a c e b y way o f t h r u s t f a u l t i n g ,
b en t fo ld in g ,
o r b o t h . B a t e s and J a c k s o n ,
re c u m ­
1980) h av e b e e n
o b s e r v e d t h r o u g h o u t A r c h e a n e x p o s u r e s i n s o u t h w e s t M ontana
(e .g . V i t a l i a n o , e t a l , 1979;
G a r ih a n , 1979).
63
5.
S y n - and p o s t - t e c t o n i c g r a n i t o i d s h a v e b e e n r e c o g n i z e d i n t h e
S p an ish Peaks a r e a
( S a l t and Mogk,
M a d iso n Range ( E r s l e v ,
6.
A rchean e x p o su re s
in
1985) an d i n t h e s o u t h e r n
1983).
so u th w e st
M ontana w e r e s u b j e c t e d
to
a
r e g i o n a l m e t a m o r p h i c e v e n t a t " 2 .7 5 B.Y. ( J a m e s a n d H e d g e ,
1980).
A s tro n g com pressio n a l te c to n ic
re g im e f o r A rchean ex p o su res in
s o u t h w e s t M o n ta n a i s i n d i c a t e d b y t h e p r e s e n c e o f g r a n u l i t e f a c i e s
r o c k s , i s o c l i n a l f o l d s , and nappe s t r u c t u r e s .
The f o l l o w i n g m o d e ls
a r e now c o n s i d e r e d t o a c c o u n t f o r t h e a b o v e - s t a t e d o b s e r v a t i o n s a n d
c o n stra in ts:
1.
W h o l e s a l e A n d e a n - ty p e s u b d u c t i o n ;
2.
C o rd ille ra n -ty p e a c c re tio n a ry te c to n ic s ;
3.
A -ty p e s u b d u c tio n , w ith o r w ith o u t l i m i t e d o cean o p e n in g .
A ndean-T ype S u b d u c t i o n
W ilso n
(1981) and F o u n t a i n and D e s m a r a is
(1980) h a v e p r o p o s e d
t h a t t h e t e c t o n i c e v o l u t i o n o f A r c h e a n r o c k s i n s o u t h w e s t M ontana c a n
be a ttr ib u te d
to
a n A n d e a n - ty p e s u b d u c t i o n r e g i m e .
S ev eral o bserva­
t i o n s made o f s t u d y a r e a r o c k s and t h o s e i n a d j a c e n t r a n g e s ,
how ever,
a r e n o t c o m p a t i b l e w i t h a l a r g e - s c a l e o c e a n i c s u b d u c t i o n m o d el.
I.
The p r e d o m i n a n c e o f s i l i c i c m e t a s e d i m e n t a r y r o c k s r e p r e s e n t e d
by s t u d y a r e a l i t h o l o g i e s and t h e s t a b l e p l a t f o r m a s s e m b l a g e s
re p re s e n te d in ranges to th e w est s h a rp ly c o n tr a s t w ith rocks
o f o cean ic
b e lts
a ffin ity .
A lth o u g h s m a l l f ra g m e n ts o f g r e e n s to n e
s u g g e s tiv e of o c e an ic c r u s t l i e
to th e so u th of th e
64
s t u d y a r e a i n t h e s o u t h e r n W yom ing p r o v i n c e
( e . g . t h e Owl
C re e k Range a s w e l l a s t h e S o u th P a s s a r e a o f t h e Wind R i v e r
R ange,
C o n d ie ,
1975),
such ro c k s have n o t b een re c o g n iz e d in
s o u t h w e s t M o ntana A rc h e a n e x p o s u r e s .
q u a rtz -th o e liitic
a m p h ib o lite s
G e o c h e m i c a l d a t a fro m
f ro m t h e T o b a c co Root Range
im p l y a c o n t i n e n t a l m a n t l e o r i g i n (H a n le y , 1 976).
tio n ,
In a d d i­
m o d al a b u n d a n c e s o f a m p h i b o l i t e u n i t s fo u n d w i t h i n t h e
p red o m in an tly q u a r tz o f e ld s p a th ic te r r a n e a re n o t s i g n i f i c a n t
e n o u g h i n v o lu m e t o b e r e g a r d e d a s o c e a n i c c r u s t .
2.
T h e r e i s an a b s e n c e o f l i t h o l o g i e s t h a t c o u l d b e i n t e r p r e t e d
as m e ta tu r b id ite s or as v o lc a n ic I a s ti c
rocks ty p ic a l of a
e u g e o c lin a l a f f i n i t y .
3.
Q u a r tz o f e ld s p a th ic g n e is s e s i n th e s tu d y a r e a a r e in p a r t Kspar ric h .
I t is su g g e ste d th a t th e so u rc e a re a fo r th e s e
r o c k s c o u l d h a v e b e e n t h e 2 .8 -2 .7 5 B.Y. g r a n i t o i d s a s s o c i a t e d
w i t h a n a n d e s i t i c a r c c o m p le x e m p la c e d i n
to o th
R ange a t
about
2 .8 B.Y..
If
s tu d y
th e e a s te rn B eararea
ro ck s w ere
i n d e e d d e r i v e d f ro m t h e s e g r a n i t o i d s , i t i s b e l i e v e d t h a t t h e
2.75 B.Y. m e t a m o r p h ic e v e n t w a s n o t o c e a n - s u b d u c t i o n r e l a t e d
a s no a r c c o m p le x o f a p p r o p r i a t e ag e e x i s t s t h a t w o u ld b e
su p p o rtiv e
of
such
a m odel
(th e
2.8
arc
co m p lex
in
th e
e a s t e r n B e a r t o o t h Range w as e m p la c e d b e f o r e t h e r o c k s i n t h e
s t u d y a r e a w e r e m e t a m o r p h o s e d a t 2.7 5 B .Y .) , a n d i s t h u s t o o
o l d t o b e a s s o c i a t e d w i t h t h e 2.75 B.Y. m e t a m o r p h i c e v e n t ) .
65
4.
L a r g e - s c a l e m a g m a tic t h i c k e n i n g o f a p p r o p r i a t e a g e , a s i g n a ­
tu re
of
A n d e a n -ty p e
su b d u c tio n
processes,
has
not
been
observ ed .
5.
A n d e a n —t y p e
su b d u c tio n
cannot
account
c r u s t a l th ic k e n in g n e c e ssa ry to
fo r
th e
am ount o f
g iv e r i s e to t r a n s i t i o n a l
g r a n u l i t e f a c i e s a sse m b la g e s w ith in ro c k s of s u p r a c r u s t a l
o r i g i n su c h as th o s e so p r e v a l e n t th r o u g h o u t A rch ean expo­
s u r e s i n s o u t h w e s t M ontana.
6.
O p h io lite seq u en ces have n o t been o b se rv e d .
The Q u e s t i o n o f A c c r e t i o n
R e c e n t r e s e a r c h i n t h e M a d iso n R ange i s h i g h l y s u g g e s t i v e o f a
c o m p le x t e c t o n i c
e v o l u t i o n o f A r c h e a n e x p o s u r e s i n s o u t h w e s t M ontana.
E r s l e v (1983) h a s r e p o r t e d t h e o c c u r r e n c e o f tw o d i s s i m i l a r l i t h o l o g i c
t e r r a n e s i n t h e s o u t h e r n M a d iso n R ange s e p a r a t e d by t h e n o r t h e a s t ­
t r e n d i n g M a d iso n m y l o n i t e z o n e .
iso to p ic
age t r a n s i t i o n zone o f G i l e t t i
P recam b rian f a u l t zone
g rap h ic
T h is zone tr e n d s p a r a l l e l to th e
o b se rv a tio n s,
(E rsle v ,
E rsle v
1983).
(1971) and r e p r e s e n t s a m a j o r
B a s e d on f i e l d
and p e t r o ­
(1983) b e l i e v e s t h a t t h e tw o d i s s i m i l a r
l i t h o l o g i c t e r r a n e s s u p p o r t s t h e h y p o t h e s i s o f tw o d i s s i m i l a r age
te rra n e s v ia te c to n ic
ju x ta p o sitio n .
Ken S a l t ( p e r s o n a l com m unica­
tio n ) has a ls o observed a b ru p t c h a n g e s i n l i t h o l o g y
grade s e p a ra te d by a m y lo n itic
S ev eral
o th e r
research ers
and m e ta m o rp h ic
s h e a r z o n e i n t h e S p a n i s h P e aks a r e a .
have
re c e n tly
p ro v id e d
d a ta
th a t
is
s u g g e s t i v e o f an a c c r e t e d t e r r a n e m odel f o r A rchean r o c k s i n s o u th w e st
M o n ta n a .
M u e l l e r e t a l (1984) h a v e fo u n d t h a t c h e m i c a l f e a t u r e s o f
66
m e ta m o r p h o s e d s u p r a c r u s t a l a s s e m b l a g e s i n t h e B e a r t o o t h d i s p l a y c h e m i­
cal
fe a tu re s
d iffe re n c es
su g g e stiv e
T hese c h e m ic a l
i n c o n j u n c t i o n w i t h l i t h o l o g i c v a r i a t i o n s and d i f f e r e n c e s
i n m e t a m o r p h ic h i s t o r y
rate
of s e p a r a te prov en an ces.
suggest t h a t th e rock s u ite s
e v o lv e d in se p a ­
a r e a s and w e r e s u b s e q u e n t l y j u x t a p o s e d t h r o u g h a c c r e t e d
processes.
te rra n e
Due t o t h e f u n d a m e n t a l d i f f e r e n c e s i n t h e n a t u r e o f s o u t h ­
w e s t M o n ta n a A r c h e a n b a s e m e n t r o c k s w i t h d o m i n a n t l y i g n e o u s r o c k s i n
t h e B e a r t o o t h Range a n d d o m i n a n t l y m e t a s e d i m e n t a r y r o c k s i n t h e r a n g e s
to th e w e s t, i t has been su g g e ste d t h a t th e a n c ie n t s i a l i c c r u s t in
t h e B e a r t o o t h Range s e r v e d a s a n u c l e u s f o r t h e a c c r e t i o n o f y o u n g e r
te rra n e s
to
Mogk, e t a l
th e w est
(M ogk, e t
a l,
in
rev ie w ;
Mogk e t
a l,
1985).
( i n r e v i e w ) h a v e p o s t u l a t e d t h a t t h e m e c h a n ism r e s p o n s i b l e
f o r t h i s j u x t a p o s i t i o n i s a n a l o g o u s on a s m a l l - s c a l e w i t h t h e t e c t o n i c
fea tu re s
d escrib ed
B u r c h f i e l and D a v i s ,
A ll
of
terran e s.
fo r
th e
C o rd ille ra
1972; Coney, e t
th e above o b s e r v a tio n s
S everal a s p e c ts
of th is
o f w e s t e r n N o r t h A m e ric a
a l,
(e.g.
1980).
a re h ig h ly s u g g e stiv e of a c c re te d
p r o b le m a r e u n c l e a r a t
F o r ex am p le, t h e r e i s th e q u e s tio n o f s c a l e .
c e rn e d w h e th e r A rchean e x p o su re s i n
th is
tim e.
I t re m a in s to be d i s ­
s o u t h w e s t M ontana r e p r e s e n t d i s ­
p la c e d t e r r a i n s v i a t e l e s c o p i n g o f one c o n tin u o u s b a s i n o r w h e th e r
a n o m a lo u s e x p o s u r e s a r e i n d i c a t i v e o f t h e e m p la c e m e n t o f e x o t i c
r a n e s b y way o f w h o l e s a l e a c c r e t i o n .
It
te r­
is p o ssib le th a t lith o lo g ie s
in th e s tu d y a r e a and in a d ja c e n t r a n g e s to th e w e s t d id n o t d e v e lo p
as a b a s in a d ja c e n t to a B e a rto o th h ig h la n d b u t w ere d e riv e d e lse w h e re
and w e re s u b s e q u e n t ly
q u e stio n
of
tim in g
ju x ta p o se d
w ith
th e B e a rto o th
m ust a l s o be c o n s id e r e d .
Range.
The
E x p o su res in so u th w e st
67
M ontana may r e c o r d
th e
o p p o s e d t o one o r o g e n y .
a c tiv ity
o f many s e p a r a t e t e c t o n i c
e v e n ts as
F o r t h i s r e a s o n i t i s q u i t e p r o b a b l e t h a t one
u n i f y i n g t e c t o n i c m o d el c a n n o t a d d r e s s a l l o f t h e p r o b le m s a s s o c i a t e d
w i t h u n d e r s t a n d i n g t h e A rc h e a n t e c t o n i c e v o l u t i o n o f t h e a r e a .
It
su res
in
is
c u rre n tly not p o ssib le to
s o u t h w e s t M o n ta n a r e p r e s e n t a l l o c h t h o n o u s
or c o lla p s e d b a sin d e p o s its .
g e o c h e m ic a l a n a ly s e s ,
and p a le o m a g n e tic
D e ta ile d
a c c re te d
terran e s
s tra tig ra p h ic re la tio n sh ip s,
a d d i t i o n a l a s w e l l a s m ore p r e c i s e a g e - d a t i n g ,
stu d ie s
a re needed in o rd e r to
th eo ry o f a c c re tio n a ry te c to n ic s
su res.
d e t e r m i n e w h e t h e r A rc h e a n ex p o ­
for
expand upon th e
S o u t h w e s t M o n ta n a A rc h e a n ex p o ­
I t i s s u g g e s t e d t h a t a c c r e t i o n o f e x o t i c t e r r a n e s may h a v e
p la y e d o n ly a m in o r r o l e i n th e t e c t o n i c e v o lu tio n o f s tu d y a r e a ro ck s
and r a n g e s t o t h e w e s t a s s t r i k e - s l i p
a c c re tio n a ry te c to n ic s
and t h i s
f a u l t i n g i s a l a r g e com ponent o f
cannot account fo r th e
g e n e ra tio n
of
t r a n s i t i o n a l - g r a n u l i t e g ra d e a sse m b la g e s.
A-Type S u b d u c t io n
F i g u r e 24 i l l u s t r a t e s
sta g e s
s u b d u c t i o n m odel f o r A r c h e a n r o c k s
o f an i n f e r r e d A -ty p e ( c o n t i n e n t a l)
in
s o u t h w e s t M o ntana.
w as p r o p o s e d by M a r tin and P o ra d a (1 9 7 7 ), M a r tin
T h is
m odel
(1 9 8 3 ), and l a t e r
p r e s e n t e d by K r o n e r (1981) to e x p l a i n t h e t e c t o n i c e v o l u t i o n o f t h e
P a n - A f r i c a n D am ara e r o g e n i c b e l t .
A firs t
s ta g e in v o lv e s th e d ep o si­
t io n of sed im e n ta ry rocks in to a i n t r a c o n t i n e n t a l o r e n s i a l i c b a s i n
(F ig u re
24 a . ) .
P la tfo rm
se d im e n ts
i n d ic a te d by th e
a sse m b la g e s
p r e s e n t i n t h e s tu d y a r e a and i n r a n g e s t o t h e w e s t (e .g . S p e n c e r and
K ozak, 1975;
V i t a l i a n o , e t a l , 1979) a r e i n d i c a t i v e o f t h e p r e s e n c e
68
a
Blacktail Range?
Tobacco Root
Range
Study area
Beartooth
Range
sea level
—
?
—
continental crust
) oceanic )
) crust? ]
upper mantle
(no scale implied)
Compression induces intracontinental subduction, high-level thrusting, and the production of nappe structures and isoclinal folds
Increased radioactive heatstg through crustal thickening and frictional heating
give rise to late and p o st-te cto n ic- metamorphic ev e n ts and po st-tecto n ic granitoids
(no scale implied)
Ruby and Tobacco
Root Ranges
S yn- and post-tecto n ic granitoids,
Spanish P eak s and the southern Madison Range
Ductile sh ear zones, Spanish P eak s,
southern Madison Range, and the
northern Gallatin Range
North Snowy Block
B eartooth Range
M etasedim entary units folded into
n ap p e com plexes and isoclinal folds
--------------------------------------1
40 miles
(app ro x im ate horizontal s c ale)
v ertical s c a le unknown
F ig u re 24.
S u g g e ste d s t a g e s in th e A rch ean t e c t o n i c e v o lu t io n of
s o u t h w e s t M ontana ( e x c l u d i n g t h e B e a r t o o t h Range) i n v o l v ­
i n g A - t y p e ( c o n t i n e n t a l ) s u b d u c t i o n . a) P r e - t e c t o n i c s e t ­
t i n g . b) C o m p r e s s io n s ! t e c t o n i c s r e s u l t i n g from A -ty p e
s u b d u c tio n (m o d ifie d from a m odel o f t h e P a n - A f ric a n
Dam ara B e l t by K r o n e r , 1981). c) S t r u c t u r a l and l i t h o l o g i c
f e a t u r e s w i t h i n s o u t h w e s t M ontana A rc h e a n e x p o s u r e s .
69
of such a b a s in .
A t t e n u a t i o n o f t h e c r u s t a c c o m m o d a te s t h e i n t r u s i o n
o f b a s a l t s w h i c h fo rm e x t e n s i v e b u t t h i n l a y e r s w i t h i n t h e m e t a s e d i ­
m en tary ro c k s.
T h is m odel i s s i m i l a r to t h a t d e s c r ib e d by S te w a rt
(1972) and E i n s e l e
u n its
fo u n d w i t h i n
(1985) t o a c c o u n t f o r t h e p r e s e n c e o f b a s a l t i c
se d im e n ta ry l i t h o l o g i e s .
L i m i t e d o c e a n i c o p e n in g
i s p o s s i b l e w i t h i n an A -ty p e s u b d u c tio n m odel (M a rtin and P o ra d a ,
1977;
M a rtin ,
1983).
A subsequent c o m p ressio n al te c to n ic
reg im e v i a
A -ty p e s u b d u c tio n in d u c e s s h o r te n in g o f th e o v e r ly in g s e d im e n ta ry
c o v e r , p r o d u c in g n a p p e c o m p le x e s and i n t e r s t a c k i n g o f s e d im e n ta r y
u n its
a l,
( F i g u r e 24 b .) .
Nappes i n t h e T ob a c co R oot Range ( V i t a l i a n o ,
1979) and t h e Ruby Range ( G a r ih a n ,
1979) t e s t i f y
to
et
th e te le s c o p ­
in g o f t h e s e d im e n ta r y c o v e r v i a l a r g e - s c a l e c o m p r e s s iv e s t r e s s e s
(F ig u re
24 c . ) .
A -ty p e s u b d u c tio n
a lso
p ro v id e s
a m ec h a n ism
fo r
s u b j e c t i n g s u p r a c r u s t a l r o c k s t o m i g m a t i z a t i o n and t r a n s i t i o n a l g r a n u —
Iite
f a c ie s c o n d itio n s as a r e s u l t o f te c to n ic th ic k e n in g v ia c r u s t a l
u n d e rth ru stin g .
An o v e r - r i d i n g o f s i a l i c p l a t e s e s t a b l i s h e s t h e c r u s ­
t a l th ic k n e sse s n ecessary fo r th e g e n e ra tio n of t r a n s i t i o n a l g r a n u lite
grade c o n d itio n s .
The d e e p c r u s t a l
le v e ls
t h a t A rchean ro c k s
in
s o u t h w e s t M ontana r e p r e s e n t c l e a r l y c o u l d n o t h a v e r e s u l t e d fro m t h i n sk in n e d t e c t o n i c s .
M y l o n i t i c s h e a r z o n e s r e s u l t f ro m i n t r a p l a t e d i s ­
p l a c e m e n t s b y way o f i n t e n s e t h r u s t i n g .
Such s h e a r z o n e s h av e b e e n
i d e n t i f i e d i n t h e S p a n i s h P e a k s ( S a l t and Mogk,
M a d i s o n R a n g e ( E r s l e v , 1 9 8 3 ; F i g u r e 24 c . ) .
1985) and t h e s o u t h e r n
Syn- and p o s t - t e c t o n i c
g r a n i t o i d s r e s u l t fro m l o w e r c r u s t a l m e l t i n g a s s o c i a t e d w i t h t e c t o n i c
t h i c k e n i n g v i a A - t y p e s u b d u c t i o n . Such m e ta m o r p h o s e d i n t r u s i v e s w i t h i n
th e
S p a n ish
Peaks
area
(S a lt
a n d M ogk,
1985) an d a m e t a - i g n e o u s
70
t e r r a n e i n t h e s o u t h e r n M a d iso n Range ( E r s l e v ,
n ize d
1983) h a v e b e e n r e c o g ­
( F i g u r e 24 c . ) .
An
in su ffic ie n t
am ount
of
d a ta
fo r
th is
area
p rec lu d es
a
th o ro u g h u n d e rs ta n d in g of th e t e c t o n i c s e t t i n g f o r A rchean ro ck s in
s o u t h w e s t M o n ta n a . T h is a u t h o r d o e s n o t d i s c o u n t t h e p o s s i b i l t y o f
o t h e r c o l l i s i o n a l m o d e ls s u c h a s o c e a n i c s u b d u c t i o n o r a c c r e t i o n a r y
t e c t o n i c s b u t s u g g e s t s t h a t a v a i l a b l e d a t a and o b s e r v a t i o n s c u r r e n t l y
b e s t s u p p o r t an A - ty p e s u b d u c t i o n m o d el o f an e n s i a l i c b a s i n .
a d d i t i o n a l g e o c h r o n o l o g i c and g e o c h e m i c a l d a t a ,
W ith
as w e ll as a d d itio n a l
f i e l d w ork, th e n a tu r e o f th e t e c t o n i c s e t t i n g f o r A rchean ro ck s in
s o u t h w e s t M o n ta n a w i l l becom e m ore c l e a r .
71
SUMMARY AND CONCLUSIONS
A rchean m eta m o rp h ic ro c k s
in
t h e n o r t h e r n G a l l a t i n Range i n
s o u t h w e s t M o ntana a r e p r e d o m i n a t l y c o m p o s e d o f r e g i o n a l l y m e t a m o r ­
p h o s e d q u a r t z o f e l d s p a t h i c g n e i s s e s w i t h m in o r a m o u n ts o f m e t a b a s i t e s ,
r e p r e s e n t a t i v e o f s u p r a c r u s t a l a s s e m b l a g e s com posed o f m e t a s e d i m e n t a r y
and m e t a v o l c a n i c r o c k s .
T h e s e r o c k s r a n g e fro m e p i d o t e —a m p h i b o l i t e t o
lo w e r g r a n u l i t e f a c i e s i n g ra d e and h av e b e e n s u b j e c t e d to i n t e n s e
d e f o r m a tio n d u r in g r e g i o n a l h ig h g ra d e m eta m o rp h ism .
E v id en ce o f
g r e e n s c h i s t f a c i e s r e t r o g r e s s i o n i n som e o f t h e r o c k s s t u d i e d
c a te s
e ith e r a se p a ra te ,
l a t e r m e t a m o r p h ic e v e n t ,
c o n d itio n s a s so c ia te d w ith a l a t e
in d i­
o r low t e m p e r a t u r e
s t a g e o f p r i o r h i g h - g r a d e m e ta m o r ­
p h is m .
M i n e r a l o g i c a l and t e x t u r a l f e a t u r e s
i n d i c a t e t h a t th e stu d y a re a
i n i t i a l l y e x p e r i e n c e d t r a n s i t i o n a l g r a n u l i t e f a c i e s m e t a m o r p h ic c o n d i ­
t i o n s u n d e r p r e s s u r e s o f 5 - 7 kb a n d t e m p e r a t u r e s o f 6 8 0 o - 7 2 0 ° .
A
re g io n a l f o li a ti o n p a r a l le l to l i t h o l o g i c
l a y e r i n g w as p ro d u c e d and
m ig m a tiz a tio n and i s o c l i n a l p a s s iv e - f lo w
f o l d s w e r e p r o b a b l y c o n te m ­
p o r a n e o u s (F l) w i t h t h i s e v e n t.
d u c e d b r o a d op en f o l d s ,
A second d e fo rm a tio n a l p e rio d p ro ­
c o a x ia l w ith F l fo ld s.
a r e a a d o m in an t s t r u c t u r a l g r a i n i s
T hroughout th e s tu d y
e x p r e s s e d by a g e n e r a l N45E t r e n d
am ongst f o l d s t r i k e s as w e l l as f o l d and l i n e a t i o n t r e n d s .
I t i s b e l i e v e d t h a t A rc h e a n l i t h o l o g i e s
i n t h e s t u d y a r e a and i n
a d ja c e n t ran g e s to th e w e st r e p r e s e n t th ic k s e d im e n ta ry sequences
72
d e p o site d
w ith in
an e n s i a l i c b a s i n .
M e ta b a site u n its w ith in th e
m e t a s e d i m e n t a r y r o c k s may r e p r e s e n t b a s a l t i c
in tru sio n s.
h i g h - g r a d e m e ta m o r p h is m s u b s e q u e n t l y a f f e c t e d
th e area.
R e g io n a l
The g e n e r a ­
t i o n o f t r a n s i t i o n a l g r a n u l i t e f a c i e s a s s e m b l a g e s an d a s s o c i a t e d m ig—
m a t i t e s , l a r g e - s c a l e i s o c l i n a l f o l d s and n a p p e s t r u c t u r e s , and d u c t i l e
sh e a r zones a t t e s t s
c r u s t a l th ic k e n in g .
to a c o m p re s sio n a l reg im e t h a t
in v o lv e d t e c t o n i c
B a s e d on a v a i l a b l e i n f o r m a t i o n and o b s e r v a t i o n s ,
t h e p r e f e r r e d m o d el f o r t h e t e c t o n i c e v o l u t i o n o f A r c h e a n r o c k s w i t h i n
th e
s tu d y a r e a and a d j a c e n t r a n g e s
( c o n t i n e n t a l ) sub d u c t i o n .
to
th e w est is
t h a t o f A -ty p e
A d d itio n a l r e s e a r c h in v o lv in g g eo ch ro n o -
l o g i c and g e o c h e m i c a l s t u d y a s w e l l a s d e t a i l e d f i e l d w o r k w i l l c o n t r i ­
b u t e t o a c l e a r e r u n d e r s t a n d i n g o f t h e t e c t o n i c e v o l u t i o n f o r A rc h e a n
r o c k s i n s o u t h w e s t M ontana.
REFERENCES CITED
74
REFERENCES CITED
A l l e n , A .R ., 1 9 7 9 , M e c h a n i s m o f f r i c t i o n a l f u s i o n i n f a u l t z o n e s .
J o u r n a l o f S t r u c t u r a l G e o lo g y , v o l . I , pp. 2 3 1 -2 4 3 .
B a t e s , R .L ., a n d J a c k s o n , J .A . ( e d i t o r s ) , 1 9 8 0 , G l o s s a r y o f G e o l o g y .
Second e d i t i o n .
A m erican G e o lo g ic a l I n s t i t u t e , F a l l s C hurch,
V i r g i n i a , 751 p.
B o u l l i e r , A .M., 1 9 8 0 , A p r e l i m i n a r y s t u d y o f t h e b e h a v i o r o f b r i t t l e
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J o u r n a l o f S t r u c t u r a l G e o lo g y , v o l . 2, no . 1 / 2 ,
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APPENDICES
83
APPENDIX A
LOCATIONS OF MAJOR OUTCROPS THAT WERE STUDIED IN DETAIL
84
APPENDIX A
O u tc ro p
Legal D e sc rip tio n
N a rra tiv e D e sc rip tio n
H -I
SW 1 / 4 , NE 1 / 4 , 23 ,
T3S, R5E
2 .3 m i l e s s o u t h a lo n g
H y a l i t e C re e k Road.
L -I
NE 1 / 4 , SE 1 / 4 , 12,
T3S, R5E
A long a b a n d o n e d l o g g i n g
F o r e s t S e rv ic e road
p a r a l l e l to L ev erich
C r e e k , 1 /3 m i l e
so u th of range f r o n t .
S/l-3"
NE 1 / 4 , NW 1 / 4 , 20 ,
T3S, R6E
1 .6 m i l e s s o u t h a lo n g
F o r e s t S e rv ic e lo g g in g
r o a d f o l l o w i n g S ourdough
C reek.
8= 1-4- "
NE 1 / 4 , NW 1 / 4 , 2 0 ,
T3S, R6E
1 .8 m i l e s s o u t h a lo n g
F o r e s t S e rv ic e lo g g in g
r o a d f o l l o w i n g Sourdough
C reek.
5>-
»-& •
85
APPENDIX B
MINERAL CONTENTS OF QUARTZOFELDSPATHIC GNEISSES
M = m ajor
am ounts
(> 5%),
Tr = t r a c e
amounts
(<
51 ), -
=not p r e se n t.
Thin s e c t io n s
HlA
Mineral
H1C2
H-3-2
H-5-4
H-9
H-IO
H-10-1
H-12-1
H-I 2-2
H-13-2
Quartz
M
M
M
M
M
M
M
M
M
-
P la g io c la s e
M
-
M
M
M
M
M
M
M
M
Kspar
-
-
-
M
-
-
M
M
-
-
Garnet
Tr
M
M
-
-
M
Tr
-
-
-
Tr
M
M
M
Tr
M
Tr
Tr
M
-
Tr
-
-
M
Tr
-
-
Tr
M
Tr
Tr
Tr
Tr
Tr
Tr
Tr
Tr
Tr
B io tite
I
Amphibole
2
Opaque phases Tr
-
Tr
-
-
-
-
-
-
-
-
M uscovite
-
-
-
-
M
-
Tr
Tr
-
-
S e r ic ite
M
-
M
M
-
-
M
Tr
Tr
Tr
group
—
—
—
—
Tr
Tr
Tr
-
Tr
Tr
Zircon
Tr
-
Tr
Tr
Tr
Tr
Tr
-
Tr
Tr
C h lo r ite
-
-
Tr
-
Tr
Tr
Tr
-
Tr
Tr
A p a tite
Tr
-
-
-
-
-
-
-
-
-
C o r d ie r ite
-
-
-
-
-
-
-
Tr
-
-
-
-
—
—
Tr
—
_
_
Tr
Epidote
S i ll i m a n i t e
1 Amphiboles are o f
hornblende com p osition u n le s s o th erw ise
2 Cummingtonite.
3 G e d r ite .
Table 5
M ineral c o n te n ts o f q u a r tz o fe ld s p a th ic g n e is s e s
in d ic a t e d .
APPENDIX B
Tourmaline
M = major amounts
O 5X).
Tr ■
not present
t r a c e amounta (< 5%)
Thin s e c t io n s
Mineral
L-5
L -U
MIG. I
S -l-2
S -l-3
S -2
S -3-1
S -3-3
S-22 S-24
S-52Gn
Quartz
M
M
M
M
M
M
M
H
P la g io c la s ^
M
M
M
M
M
M
M
M
Kspar
Tr
-
M
M
M
M
M
Garnet
-
-
-
Tr
-
Tr
Tr
B io tite
M
M
-
M
M
M
M
Amphibole
-
M
-
-
-
M
phases
Tr
Tr
Tr
Tr
Tr
Tr
Tourmaline
-
-
-
-
-
Tr
M uscovite
Tr
-
-
Tr
Tr
Tr
Tr
M
S e r ic ite
M
M
M
Tr
Tr
H
M
M
group
Tr
Tr
Tr
Zircon
-
Tr
Tr
Tr
Tr
Tr
Tr
Tr
C h lo r ite
Tr
Tr
M
-
-
Tr
Tr
Tr
A p a tite
-
-
-
-
-
Tr
C o r d ie r ite
-
Tr
-
-
-
Tr
Tr
Tr
H
Tr
Opaque
CO
*vl
Epidote
Sillimanite
Tr
Tr
Tr
APPENDIX C
MINERAL CONTENTS OF AMPHIBOLITE FACIES '
M = major amounts (> 5%),
Tr = trace amounts (< 5%).
- = not present.
Thin s e c t io n s
H-1B3
Mineral
H-IE
H-A
H-5-1
H-6
H-7
L-7
L - 19
MIG2
M
GU
M
H
M
M
M
S - 1-1
S -3-2
S -3-4
S-6
S-52
M
M
M
3
2
I
L-IO
M
M
H
H
M
M
M
P la g io c la s e
H
M
M
M
-
M
-
-
M
Tr
M
M
M
M
M
M
Garnet
M
-
M
-
M
-
-
-
-
-
M
M
M
M
-
M
Quartz
M
-
M
-
Tr
M
-
-
Tr
H
Tr
M
Tr
T
M
-
B io tite
Tr
-
Tr
Tr
-
-
Tr
Tr
M
-
-
Tr
M
M
M
Tr
-
M
-
-
-
-
-
-
-
-
-
-
-
-
-
-
phases
Tr
Tr
Tr
Tr
M
Tr
M
M
Tr
-
Tr
Tr
M
Tr
Tr
Tr
Sphene
H
-
Tr
Tr
-
Tr
-
-
-
-
M
Tr
-
Tr
-
-
group
-
-
-
-
-
Tr
-
-
-
Tr
Tr
Tr
-
-
Tr
-
Zircon
Tr
Tr
-
Tr
-
-
-
-
-
Tr
-
Tr
-
Tr
Tr
Tr
C h lo r ite
Tr
-
-
-
-
-
Tr
Tr
Tr
M
-
-
Tr
Tr
-
-
S e r ic ite
H
M
Tr
-
-
M
Tr
-
-
-
M
Tr
-
M
M
-
A p a tite
-
-
Tr
Tr
-
-
-
-
-
-
Tr
-
-
-
-
-
M
C lin o pyroxene
Opaque
Epidote
1 Amphiboles
are o f
hornblende com p osition u n le s s
o th er w ise
2 Cummingtonite and t r e m o l i t e .
3 A c tin o lite .
Table b .
M ineral c o n te n ts o f a m p h ib o lite f a c ie s
in d ic a t e d .
APPENDIX C
Amphibole
90
I
APPENDIX D
MINERAL CONTENTS OF TRANSITIONAL GRANULITES
M = major amounts (> 5X).
Tr = trace amounts (< 5%).
- = not present.
Thin s e c t io n s
5-/3
M inerals
L-A
L-12
S-13
S-52A
Hornblende
M
M
M
M
M
P la g io c la s e
M
M
M
M
M
B io tite
-
Tr
Tr
-
Tr
Quartz
M
-
M
-
-
Garnet
M
-
-
-
M
M
M
M
M
M
phases
Tr
Tr
Tr
Tr
Tr
Sphene
Tr
-
Tr
-
-
Zircon
-
-
Tr
Tr
-
S e r ic ite
-
Tr
Tr
M
-
C h lo r ite
-
Tr
-
Tr
-
-
M
-
-
-
C lin o pyroxene
Opaque
Epidote
group
Table 7 .
M ineral c o n te n ts o f t r a n s it io n a l g r a n u lit e s .
APPENDIX D
H-27-1
MONTANA STATE UNIVERSITY LIBRARIES
IliI I
762 IOO 4943 2
Main
B378
MUU7
cop.