GEOL 3313 Petrology of Igneous and Metamorphic Rocks Study Guide for Final Examination Glen Mattioli

Similar documents
Metamorphic Petrology. Jen Parks ESC 310, x6999

Types of Metamorphism!

Archean Terranes. Archean Rocks. Southeastern Africa. West Greenland. Kaapvaal Craton. Ancient Gneiss Complex

Metamorphic Energy Flow. Categories of Metamorphism. Inherited Protolith Character. Inherited Fabric. Chemical Composition

Big Island Field Trip

Chapter 4 Rocks & Igneous Rocks

Metamorphism and Metamorphic Rocks

Lecture 5 Sedimentary rocks Recap+ continued. and Metamorphic rocks!

Introduction. Introduction. Chapter 7. Important Points: Metamorphism is driven by Earth s s internal heat

Chapter 21: Metamorphism. Fresh basalt and weathered basalt

Chemical Systems. Introduction to Metamorphism. Definition of Metamorphism. Lower Limit of Metamorphism. Upper Limit of Metamorphism

Trace Elements. Today s lecture

5/1/2017. Why Study Metamorphism? The Limits of Metamorphism. Low-temperature limit grades into diagenesis. Intro. to Metamorphism

GLY 155 Introduction to Physical Geology, W. Altermann. Grotzinger Jordan. Understanding Earth. Sixth Edition

Igneous Rocks. Igneous Rocks. Genetic Classification of

Chapter 8 Lecture. Earth: An Introduction to Physical Geology. Twelfth Edition. Metamorphism. Rocks. Tarbuck and Lutgens Pearson Education, Inc.

Igneous and Metamorphic Rock Forming Minerals. Department of Geology Mr. Victor Tibane SGM 210_2013

Imagine the first rock and the cycles that it has been through.

Metamorphism and metamorphic rocks. GEOL115 Alexander Lusk

Chapter 21: Metamorphism. Fresh basalt and weathered basalt

Constitution of Magmas. Magmas. Gas Law. Composition. Atomic Structure of Magma. Structural Model. PV = nrt H 2 O + O -2 = 2(OH) -

Chapter 7 Metamorphism, Metamorphic Rocks, and Hydrothermal Rocks

Structure of the Earth and the Origin of Magmas

Lecture 25 Subduction Related Magmatism

Igneous Rocks of the Convergent Margins

Introduction to Geology Spring 2008

Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100

N = N 0 e -λt D* = N 0 -N D* = N 0 (1-e -λt ) or N(e λt -1) where N is number of parent atoms at time t, N 0

GY303 Igneous & Metamorphic Petrology. Lecture 7: Magma Sources and Tectonic Environments

Engineering Geology ECIV 2204

Rare Earth Elements in some representative arc lavas

Chapter 4 8/27/2013. Igneous Rocks. and Intrusive Igneous Activity. Introduction. The Properties and Behavior of Magma and Lava

Understanding Earth Fifth Edition

GEOL 2312 Igneous and Metamorphic Petrology Spring 2009 Sc ore / 40

GEOL 2312 Igneous and Metamorphic Petrology Spring 2016 Score / 58. Midterm 1 Chapters 1-10

Lecture 14: A brief review

Estimated ranges of oceanic and continental steady-state geotherms to a depth of 100 km using upper and lower limits based on heat flows measured

Lab: Metamorphism: minerals, rocks and plate tectonics!

Plate tectonics, rock cycle

2 Britain s oldest rocks: remnants of

EENS 2120 Petrology Prof. Stephen A. Nelson. Types of Metamorphism

Florida Atlantic University PETROLOGY -- MIDTERM TWO KEY

Overview of the KAHT system. Ian E.M. Smith, School of Environment, University of Auckland

Ultramafic rocks. Types of Ultramafic Rocks. Spinel lherzolite xenolith

Earth and Space Sciences 212

Essentials of Geology, 11e

Metamorphic Facies. Fig Temperaturepressure

Metamorphic Petrology GLY 262 Metamorphic fluids

Metamorphism: Alteration of Rocks by Temperature and Pressure

The Nature of Igneous Rocks

Effect of tectonic setting on chemistry of mantle-derived melts

Worked Example of Batch Melting: Rb and Sr

Metamorphism (means changed form

CHAPTER VI CONCLUSIONS

Differentiation 2: mantle, crust OUTLINE

Definition: Metamorphic rocks: Remember the Rock Cycle

Factors cause Metamorphism:

Metamorphic Rocks. Metamorphic rocks. Formed by heat, pressure and fluid activity

Metamorphism: summary in haiku form

1 Potassic adakite magmas and where they come from: a mystery solved?

Metamorphism. Metamorphic Rocks. Sources of Heat for Metamorphism. Sources of Heat for Metamorphism. in mineral assemblages of a rock, and/or

1 F 4. Greenschist-amphibolite facies, such as those of Western North Carolina, require an average continental crustal geotherm to form.

Origin of Basaltic Magma. Geology 346- Petrology

Chapter 8 10/19/2012. Introduction. Metamorphism. and Metamorphic Rocks. Introduction. Introduction. The Agents of Metamorphism

Metamorphism / Metamorphic Rocks

Lecture 3 Rocks and the Rock Cycle Dr. Shwan Omar

Metamorphic Petrology GLY 262 Metamorphism and plate tectonics

Petrology Session 2. Metamorphism: Alteration of Rocks by Temperature and Pressure

"When Gregor Samsa woke up one morning from unsettling dreams, he found himself changed into a monstrous bug. Metamorphosis, by Franz Kafka

Earth Science 232 Petrography

Igneous Rock. Magma Chamber Large pool of magma in the lithosphere

UNIVERSITY OF EDINBURGH. College of Science and Engineering School of GeoSciences. Earth Materials UO4824 DEGREE EXAMINATION (MOCK) xxxxxxxxxxxxxxxxx

16. Metamorphic Rocks II (p )

Lab 6: Metamorphic Rocks

Metamorphic Rocks. Metamorphic Rocks: Big Ideas

Igneous Rocks. Definition of Igneous Rocks. Igneous rocks form from cooling and crystallization of molten rock- magma

Engineering Geology. Metamorphic Rocks. Hussien Al - deeky

Classification and Origin of Granites. A Multi-faceted Question

Metamorphism and Metamorphic Rocks Earth - Chapter Pearson Education, Inc.

Introduction. Volcano a vent where molten rock comes out of Earth

Metamorphic Petrology

Introduction. Introduction. Introduction 10/15/2014. The Agents of Metamorphism. Metamorphism. and Metamorphic Rocks

Questions on the characteristics and generation of subduction-related andesitic magmas at convergent margins (not covered on Midterm exam)

How 2 nd half labs will work

ד"ר חנן גינת ד"ר ירון פינצי

Metamorphic Petrology GLY 262 P-T-t paths

1. are most likely to study the images sent back from Mars. A. Astronomers B. Geologists C. Doctors D. Engineers

Chapter 18: Granitoid Rocks. Chapter 18: Granitoid Rocks. Melting of crustal materials at high pressure

Rocks: Materials of the Solid Earth

12 Chemistry (Mg,Fe) 2 SiO 4 Olivine is forms what is called an isomorphous solid solution series that ranges between two end members: Forsterite Mg

Lecture 2: Causes of metamorphism

GSA Data Repository

Chapter - IV PETROGRAPHY. Petrographic studies are an integral part of any structural or petrological studies in

Progressive Metamorphism. Progressive Metamorphism. P-T-t t Path. Prograde Reactions. Progressive Metamorphism. Types of Protolith

Igneous activity is related to convergent plate situations that result in the subduction of one plate beneath another Ocean-ocean Island Arc

Hornblende (Ca,Na)2-3(Fe,Mg,Al)5Si6(Si,Al)2O22(OH)2. Kaolinite (clay) Al2Si2O5(OH)4. Foliation ANIMATION

Partial melting of mantle peridotite

Earth Science 11: Earth Materials: Rock Cycle

Lesson Seven: Metamorphic Rocks

Lecture 6 - Igneous Rocks and Volcanoes

Transcription:

GEOL 3313 Petrology of Igneous and Metamorphic Rocks Study Guide for Final Examination Glen Mattioli Chapter 5: Crystal-Melt phase diagrams Effect of water pressure on feldspar stability Hypersolvus vs. sub-solvus granites o Petrographic/Mineralogic characteristics o Binary phase relations Ternary Phase Diagrams o An-Ab-Kf o Intersection of liquidus surface o Thermal Valley o Solvus or miscibility gaps Ternary feldspar tie-lines Natural feldspar compositions o Rhyolite pumice o Trachybasalt Liquid line of descent: effect of late stage xtals Water saturated ternary equilibria o Effect of pressure o Comparison with natural modes Models for the origin of Granites o Fractional crystallization o Assimilation o Magma mixing o Sub-solidus recrystallization Pyroxene quadrilateral Mica and amphibole melt equilibria: effect of fo 2 Thermal stability of volatile minerals (see again for met-pet) Assessing disequilibrium o Grain shape o Reaction rims o Compositional zoning o Inappropriate phases Chapter 6: The Mantle (from Hess) Internal Earth structure pie diagram o Crust o Mantle Upper Transition Zone Lower o Core

Outer core Inner core Internal Earth divisions o Depths o Volumes o Mass Comparison of Earth with other terrestrial planets Seismic wave velocity and density with depth End-member mantle convection models o Whole mantle o 2 layer convection Trace element concentrations o Solar atmosphere concentrations o C1 carbonaceous chondrites vs. solar photosphere Bulk Earth chemical models o Pyrolite o Model mantle o Core Schematic rift structure o Relationship to mantle melting/upwelling o Lithosphere/Asthenosphere boundary o 800 C isotherm Peridotite textures Mantle xenoliths o Modes of mantle minerals o Major element compositions of sp vs. gt. Peridotites o Hydrous mineral compositions MgO vs. major element variation diagrams Depletion vs. Fertility Trace element characteristics o REE patterns Decoupled major and trace element concentrations Chapter 11: Generation of Magma Causes of mantle melting o Temperature o Pressure o Fluids Melting environments for Oceanic lithosphere Melting environments for Continental lithosphere Peridotite melting relations Volatile-free primordial mantle composition Mantle metasomatism o Affect on major elements o Trace elements o Isotopes

Melt interfacial angles Di-Fo-Qtz phase relations and MORB generation o Effect of CO 2 pressure Fractional vs. Batch (equilibrium) melting Alkali basalt generation o Effect of CO 2 and H 2 O pressure on melt composition o Effect of melt fraction Trace element fractionation systematics o Derived liquid o Residual solid REE patterns of low degree partial melts Melt generation in a metasomatized mantle Melt generation in the continental crust Melt segregation o Effect of volume o Melting process o Syndeformational melting -> migmatites (see met-pet) Chapter 7 and 8: Primary melts and MORB generation (from Hess) Mantle melts: definitions o Primary melts o Primative melts o Parental melts Low pressure vs. high pressure multiple saturation Trace and major element characteristics of primary mantle melts Tests for whether a melt is primary Spreading center profiles o Slow Atlantic o Fast Pacific Thickness and P-wave velocity of oceanic crust FAMOUS glass compositions AMAR valley MgO variation diagrams Characteristics (major element) of plag., cpx, olivine fractionation Compatible trace element behavior vs. Mg. Number REE variations o N-MORB (normal) o T-MORB (transitional) o E-MORB (enriched) Sm/Nd and Rb/Sr isotopic variations The mantle array HSFE/LILE patterns Consensus model for MORB generation Chapter 10 and 11 (Hess) and Chapter 12 and 13 (Best) Tectonic distribution of modern island arcs Schematic island arc cross-section

AFM plots o Calc-alkaline trend o Tholeiite trend K 2 O vs. SiO 2 trends for modern island arcs o Low-K series o Calc-alkaline series o High-K series o Shoshonite series Generalized phenocryst assemblages for island arc series Average compositions for island arc series o Major elements o Trace elements o SiO 2 variation diagrams o REE concentrations vs. Mg# e-nd vs. e-sr: comparison of island arcs with the Mantle Array Pb-Pb isotopes and the need for minor continental sediment input Trace element characteristics of altered MORB and sediments Andean volcanism Generalized composition of basaltic andesites Plutons of the Sierra Nevada, Peninsular Ranges and the Canadian Pacific Northwest Major and trace element zonation in the Sierra Nevada batholiths Sr-isotopic contours in the Sierra Nevada batholiths Chapter 14: Metamorphic Rocks and Metamorphism Metamorphic driving forces P-T conditions of metamorphism Relationship of metamorphism with plate tectonics Simple definitions: o Metamorphism o Diagenesis o Melting Equilibration in metamorphic rocks features o Preservation of relic textures o Recrytallization o Increase in grain size o Crystallization of new minerals and fabrics o Tectonites Before and after metamorphism: volcanic tuff example Hydrothermal breakdown of primary igneous minerals Relic phenocrysts Ostwald ripening: grain size growth with time Prograde thermal metamorphism, an example: o Diabase o Greenstone o Amphibolite

o Granofels Textural Definitions o Porphyroblastic o Poikiloblasts o Epitaxial growth o Cataclasis o Tectonites Foliations Lineations Fractal nature of deformation Tectonic fabric development in greywacke Cleavage formation o Slaty cleavage o Crenulation cleavage o Cleavage Transposition Examples of ductile metamorphism o Undeformed Archean pillow basalts o Highly deformed and sheared pillows Recognition of metamorphic protoliths o Relic fabrics o Field relations o Bulk chemistry Global average shale composition End-member protoliths o Ultramafic o Mafic o Quartzo-feldspathic o Calc-silicate and calcareous o Ferruginous Factors controlling metamorphism o Temperature o Pressure o Fluids o Deviatoric stress Schematic Continental convergent margin and its relationship to metamorphism Chapter 12 continued: Metamorphic Terranes, Facies, and Reactions Generalized metamorphic terranes o Ocean ridge o Regional o Burial o Contact o Dynamic shear o Impact Prograde vs, Retrograde metamorphic pathways o Decarbonation

o Dehydration Onawa Contact Metamorphic Aureole o Changes in composition o Changes in texture o Relationship with fluids and heat Examples of Retrograde metamorphism o Eclogite o Epidote veins in granodiorite Crestmore felsic metamorphic intrusion and skarn: changes in mineralogy o Low grade: Forsterite zone o High grade: Garnet zone Scottish Barrovian zones in pelites Index minerals and isograds Metamorphic facies and field gradients Facies reactions Pressure-Temperature-Time paths Progressive ductile deformation Polymetamorphism L-S tectonite fabrics Pressure solution and volume loss: formation of spaced cleavage Compatibility diagrams o No solid solution o With solid solution AFC composition diagrams AFM projection diagrams Overview of metamorphic mineral reactions o Solid-solid o Solid-Fluid o Discontinuous reactions o Continuous reactions Basalt -> Granulite -> Eclogite transition Compositional effects on mineral stability: ACF in granulites Devolatilization reactions