The Results of macrofaunal analysis of rock samples from the well
№ 4-С of Vakskaya area
Example 3. Depth 86-100 m.
 Globigerina officinalis Subb.
 Globigerinella micra (Coli)
 Bulivina budensis (Hent)
 B. achalsichensis Katsch.
 Acarinina rugoscaculeata Subb.
Olygocene
Example 1. Depth 100-115 m.
 Gyroidina soldanil Orb.
 Anomalina scuta Plumm.
 Rotalia postinermis Katsch.
 R. Georgiana Katsch.
 Uvigerina jacksonensis Cush.
 Globigerina bulloides (Orb.)
 G. eocaenica Terg.
 Globigerinoides conglobatus (Brady)
Upper Eocene
Example 5. Depth 115-140 m.
 Valvulineria Iphigenia Sam.
 Planulina costatus (Hant)
 Eponides umbonatus (Rss)
 Cibicides dutemplei (Orb)
 Globigerina eocaenica Terg.
 G. bulloides Orb.
 Globigerinoides index Fihl.
 G. conglobatus (Brady)
 Nonion soldanii (Orb.)
 Asterigerina bracteata Cush.
Upper Eocene
Example 6. Depth 140-160 m.
 Spiroploctamina longa Katsch.
 Gyroidina soldanii (Orb.)
 Eponides umbonatus (RSS)
 Valvulineria angulata Katsch.
 V. palmarealensiformis Katsch.
 Pseudoplanulina meskhethica Katsch.
 Asterigerina bracteata Cush.
 Globigerina bulloides (Orb.)
 G. triloculinoides Plumm.
 Globigerinoides conglobatus (Brady)
Upper Eocene
Leader of paleontological group
Micropaleontologist
Z. Imnadze
Goderdzishvili
The Results of macrofaunal analysis of rock samples from the well
№ 4-С of Vakskaya area
Depth 115-140 m. Example №5
Prints Pitar sp.
Prints Corbulla? (gibba) Oil
Khadum?
/Kalykhanova/
Well
№ 5-С
The description of core sample from the well №5-С of Vakskaya area
Coring period
From
To
1
2
0
18
Recovery, m.
Description of rocks
3
3.00
4
Grey-yellow, fine-grained, weakly micaceous sand
with a low content of gravel.
Boulders of igneous rocks and sediments.
Green-grey, fine-grained, solid, firm, noncarbonate, weakly micaceous sandstone.
Sandstone is the same.
Beneath – grey and foxy-red, fine-grained, firm,
fractured, partly ironshot sandstone, below – darkgrey with a greenish tint, dense, non-carbonate,
sandy, weakly micaceous clay rich in fish scale.
Dark-grey with a greenish tint, stratified, noncarbonate, sandy, weakly micaceous clay with fish
scale.
The same clay with two dark-grey, firm, cavernous
bands of limestone containing druses of tiff.
Dark-grey, dense, non-carbonate, sandy, weakly
micaceous clay with fish scale.
Light-grey, fine-grained, solid, non-carbonate,
weakly micaceous sandstone of medium strength.
Dark-grey, dense, stratified, non-carbonate, sandy,
weakly micaceous clay with fish scale.
Clay is the same.
Clay is the same.
Clay is the same.
Clay is the same.
Clay is the same; at the bottom of the core sample
- dark-grey, fine-crystalline, firm limestone with
druses of tiff.
Clay is the same; at the top of the core sample
limestone is similar to the above-mentioned. Some
organic residues are present.
Dark-grey, dense, non-carbonate, aleurite, weakly
micaceous clay; at the bottom of the core sample –
a dark-grey, dense, firm limestone band.
The same clay with a dark-grey, dense, firm
limestone band.
Clay is the same; partly ironshot.
Clay is the same.
Dark-grey, dense, stratified, non-carbonate, sandy,
weakly micaceous clay rich in fish scale and other
organic residues.
Clay is the same; partly sandier.
Clay is the same
Clay is the same
Clay is the same, with fish scale.
Clay is the same; at the bottom of the core sample
– a thin band of dark-grey, firm, dense limestone.
Clay is the same
18
106
106
109
9.00
1.50
109
114
2.50
114
120
4.00
120
141
3.00
141
147
1.00
147
151
4.00
151
152
1.00
152
155
156
158
159
155
156
158
159
161
3.00
1.00
1.00
1.00
2.00
161
163
2.00
163
166
3.00
166
169
3.00
169
170
175
170
175
179
1.00
4.00
4.00
179
183
185
187
192
183
185
187
192
195
4.00
2.00
2.00
4.00
3.00
195
196
1.00
196
200
4.00
200
202.5
205
208
210
211
213
202.5
205
208
210
211
213
215
1.00
2.00
2.00
1.00
1.00
1.00
1.00
Dark-grey with a greenish tint, dense, noncarbonate, sandy, weakly micaceous clay rich in
fish scale.
Clay is the same
Clay is the same
Clay is the same
Clay is the same, but sandier and less dense.
Clay is the same
Clay is the same
Clay is the same
V. Krutovskaya