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Petrology b The study of the properties of rocks and the processes behind their formation b Recognition and description of rocks b Interpretation of their origin and history
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Instructor b Michael F. Sheridan b email: mfs@geology.buffalo.edumfs@geology.buffalo.edu b Homepage: http://www.eng.buffalo.edu/~mfshttp://www.eng.buffalo.edu/~mfs b Office hours: We & Th 1:00-2:00 PMWe & Th 1:00-2:00 PM
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Fundamentals b Classification b Changing States (Equilibrium) b Plate Tectonics & Petrology b Thermodynamics b Kinetics
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Magmatic Rock Bodies b Study of rocks in hand sample b Descriptive Petrochemistry b Origin and evolution of magmas b Interpretative Petrochemistry
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Study of rocks in hand sample b Fabric b Rock forming minerals b Classification
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Fabric b Phaneritic b Aphanitic b Glassy b Clastic
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Sequence of mineral formation b Degree of perfection of form b Inclusion within other minerals b Chemical zonation b Signs of deformation b Secondary growth b Alteration to secondary minerals
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Rock forming minerals b Feldspars b Quartz b Pyroxenes b Olivines b Amphiboles b Micas b Feldspathoids
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Classification b Leucocratic b Felsic b Silicic b Mafic b Ultramafic
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Rock Suites b Mafic and ultramafic b Calc-alkaline b Highly alkaline
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Descriptive Petrochemistry b Chemical analyses Major elementsMajor elements Trace elementsTrace elements b Relation of chemistry to mineralogy
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Chemical classification b Silica concentration Acid >66%Acid >66% Intermediate 52-66%Intermediate 52-66% Basic 45-52%Basic 45-52% Ultrabasic <45%Ultrabasic <45%
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Silica saturation b Oversaturated compatible with quartzcompatible with quartz b Saturated Neither undersaturated minerals nor quartzNeither undersaturated minerals nor quartz b Undersaturated undersaturated mineralsundersaturated minerals
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Alkali/Aluminum saturation b Relative to feldspar composition NaAlSi 3 O 8NaAlSi 3 O 8 b Peralkaline b Peraluminous b Calc-alkaline
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CIPW norm b Definition b How calculated b Use in classification
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Chemistry of rocks b Major elements b Trace elements b CIPW norm
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From Mineral Composition to Rock Composition b Determine the minerals present b estimate their abundance b Calculate the rock composition using proper weightings
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Interpretative Petrochemistry b Models of crystallization b Concepts of magma movement b Secondary alteration
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Ultramafic rock bodies b Petrography of gabbroic and ultramafic rocks b Nature of Plutons b Oceanic subalkaline basaltic to ultramafic associations b Ophiolites
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Petrography of gabbroic and ultramafic rocks b General phaneritic grain sizephaneritic grain size may be nearly monomineralicmay be nearly monomineralic –Pyroxene –Olivine –Plagioclase b Fabric Slow sequential growthSlow sequential growth Hypidiomorphic granularHypidiomorphic granular
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Petrography of gabbroic and ultramafic rocks b Classification b Alteration deuteric and hydrothermal alterationdeuteric and hydrothermal alteration SerpentineSerpentine Secondary iron oxideSecondary iron oxide brucite & talcbrucite & talc
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Nature of Gabbroic Plutons b Dikes, sills, and plugs b Layered intrusions b Slow shallow cooling of basaltic magma
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