GEOL 2312 IGNEOUS AND METAMORPHIC PETROLOGY Lecture 2 Classification of Igneous Rock or How many ways can you skin a rock? Jan. 23, 2009 GOALS OF A ROCK CLASSIFICATION SCHEME Practical – especially for field use Descriptive – minimal genetic terms Systematic – allows for easy information retrieval Hierarchical – allows for greater levels of detail Natural – defines boundaries that agree with nature Most common schemes based on mode (vol. %) of “essential” primary minerals ... (When observation of primary minerals is not possible (e.g., too fine, altered) chemistry is commonly used) ...with modification by texture and structural features and occurrence of “accessory” and minor minerals “ESSENTIAL” MINERALS Basic Spinel LIGHT MINERALS •Leucocratic •Felsic Minerals Synonymous Terms Synonymous – Terms DARK MINERALS •Melanocratic •Mafic Minerals Color Index-CI =% Dark Minerals Acid A SIMPLE (BUT LIMITING) CLASSIFICATION SCHEME CLASSIFICATION OF PHANERITIC MAFIC IGNEOUS ROCKS RECOMMENDED BY THE IUGS* gabbro troctolite Ol gabbro *International Union of Geological Sciences PLOTTING ON TERNARY DIAGRAMS Rock A Mineral X – 59.5% Mineral Y – 17% Mineral Z – 8.5% Mineral A – 12% Mineral B – 3% Normalization to XYZ only X+Y+Z = 85% Xn = 59.5/85 = 70% Yn = 17/85 = 20% Zn = 8.5/85 =10% CLASSIFICATION OF ULTRAMAFIC IGNEOUS ROCKS RECOMMENDED BY IUGS Olivine Dunite 90 Peridotites Lherzolite 40 Pyroxenites Olivine Websterite Orthopyroxenite 10 Websterite 10 Orthopyroxene Clinopyroxenite Clinopyroxene MAFIC ROCK CLASSIFICATION SCHEMES APPLIED TO THE DULUTH COMPLEX Streckeisen (1976) Phinney (1972a) LeMaitre (1989) Davidson (1969a) Severson and Hauck (1990) ELEMENTS OF A PRACTICAL CLASSIFICATION SCHEME FOR DULUTH COMPLEX MAFIC ROCKS - uses all five major essential mineral phases (Pl, Ol, Cpx, Opx, and Feox) - defines modal boundaries that bracket natural modal populations and cotectic proportions determined from experimental data - uses simple mafic mineral ratios (3:1 or 1:1) which are easy to estimate in the field. From Miller (1986) PREFERRED MODAL CLASSIFICATION MODIFIERS – FOR A COMPLETE ROCK DESCRIPTION Alteration Foliation/Layering Absolute Grain Size Bulk Rock Texture –based on pyroxene habit Accessory/Minor Minerals For example: Serpentinized, modally layered, medium-grained, subophitic, biotitic, oxide-bearing TROCTOLITE Why PYROXENE-BASED BULK-ROCK TEXTURES? Ophitic-Subophitic Ophitic Subophitic Intergranular Pl Ol CLASSIFICATION OF INTERMEDIATE AND FELSIC ROCKS Intermediate (“ferro-”) Felsic Root Rock Name From Streckeisen (1976) Attach mafic mineral prefix to root rock name for intermediate rocks... or “ferro” if uncertain of mafic mineral phase THE MAFIC TO INTERMEDIATE TRANSITION Typically based on average An content (> or < An50) Hyndman (1972) suggests also considering: rock associations (diorite with more granitoid rocks, gabbro with more mafic rocks) mafic mineral assemblage (diorite = hornblende or biotite pyroxene; gabbro = pyroxene olivine hornblende) plagioclase color (diorite whitish or nearly so; gabbro - greenish gray to gray) Blatt and Tracy (1995) suggest using diorite for rock that contains hornblende over pyroxene and that contain less than 35 modal percent high-temperature mafic minerals (olivine, pyroxene). Problems Can’t “see” AN content in hand samples Even DC felsic rocks are dominated by pyx over hb and bio Suggested Field Criteria for DC Intermediate Dark Mineral Habit Felsic Mesostasis prismatic, subprismatic >5 % Mafic granular to poikilitic <5 % Q CLASSIFICATION OF VOLCANIC ROCKS RECOMMENDED BY THE IUGS 60 60 Rhyolite Dacite 20 20 Basalt/Andesite Distinctions Trachyte SiO2 Basalt < 52% Andesite > 52% CI > 35% < 35% Foid Minerals Nepheline Leucite Kalsilite Analcime Sodalite Latite 35 A 10 (foid)-bearing Trachyte Andesite/Basalt 65 (foid)-bearing Latite Phonolite (foid)-bearing Andesite/Basalt 10 Tephrite 60 60 (Foid)ites F P CHEMISTRY-BASED TAS CLASSIFICATION OF APHANITIC OR METAMORPHOSED IGNEOUS ROCKS CIPW NORMATIVE CALCULATIONS PSEUDOMINERALOGY Calculated from whole rock geochemical analyses; distributes major elements among rock-forming minerals CLASSIFICATION OF PYROCLASTIC ROCKS