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9781405105880

Igneous and Metamorphic Petrology

by
  • ISBN13:

    9781405105880

  • ISBN10:

    1405105887

  • Edition: 2nd
  • Format: Paperback
  • Copyright: 2002-12-13
  • Publisher: Wiley-Blackwell

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Summary

Igneous and metamorphic petrology has over the last twenty years expanded rapidly into a broad, multifaceted and increasingly quantitative science. Advances in geochemistry, geochronology, and geophysics, as well as the appearance of new analytical tools, have all contributed to new ways of thinking about the origin and evolution of magmas, and the processes driving metamorphism.This book is designed to give students a balanced and comprehensive coverage of these new advances, as well as a firm grounding in the classical aspects of igneous and metamorphic petrology. The emphasis throughout is on the processes controlling petrogenesis, but care is taken to present the important descriptive information so crucial to interpretation. One of the most up-to-date synthesis of igneous and metamorphic petrology available. Emphasis throughout on latest experimental and field data. Igneous and metamorphic sections can be used independently if necessary.

Author Biography

Myron G. Best is Professor Emeritus at Brigham Young University, is a Fellow of the Geological Society of America, and a member of the American Geophysical Union.

Table of Contents

Preface
Overview of Fundamental Concepts
Energy and the Mantle Heat Engine
2(8)
Forms of Energy
2(1)
Flow and Transformation of Energy
3(1)
Heat Flow in the Earth
3(5)
Implications of Mantle Convection
8(1)
Energy Budget of the Earth
9(1)
Gravity, Pressure, and Geobaric Gradient
10(1)
Rock-Forming Processes as Changing States of Geologic Systems
10(1)
Rock Properties and Their Significance
11(3)
Composition
12(1)
Field Relations
13(1)
Fabric
14(1)
How Petrologists Study Rocks
14(2)
Composition and Classification of Magmatic Rocks
Analytical Procedures
16(6)
Sampling
16(1)
Analyses
17(5)
Mineral Composition of Magmatic Rocks
22(1)
Glass
22(1)
Chemical Composition of Magmatic Rocks
23(2)
Variation Diagrams
23(1)
Continuous Spectrum of Rock Compositions
24(1)
Classification of Magmatic Rocks
25(12)
Classification Based on Fabric
27(1)
Classification Based on Field Relations
27(1)
Classification Based on Mineralogical and Modal Composition
28(2)
Classification Based on Whole-Rock Chemical Composition
30(5)
Rock Suites
35(2)
Classification of Basalt
37(1)
Trace Elements
37(7)
Partition Coefficients and Trace Element Compatibility
38(2)
Rare Earth Elements
40(2)
Other Normalized Trace Element Diagrams
42(2)
Isotopes
44(7)
Stable Isotopes
44(1)
Radiogenic Isotopes
45(2)
Cosmogenic Isotopes: Beryllium
47(4)
Thermodynamics and Kinetics: An Introduction
Why Is Thermodynamics Important?
51(1)
Elementary Concepts of Thermodynamics
52(4)
Thermodynamic States, Processes, and State Variables
52(1)
First Law of Thermodynamics
53(1)
Enthalpy
53(1)
Entropy and the Second and Third Laws of Thermodynamics
54(1)
Gibbs Free Energy
55(1)
Stability (Phase) Diagrams
56(3)
Slope of the Melting Curve
57(1)
Determination of Phase Diagrams
58(1)
Thermodynamics of Solutions: Some Basic Concepts
59(2)
Components and Mole Fractions
59(1)
Partial Molar Volume
59(1)
Partial Molar Gibbs Free Energy: The Chemical Potential
60(1)
P-T-X Phase Diagram
61(1)
Application of Thermodynamics to Solutions
61(5)
Fugacity and Activity
61(1)
Equilibrium Constants
62(1)
Silica Activity, Silica Buffers, and Silica Saturation
63(1)
Oxygen Buffers
64(2)
Fe-Ti Oxide Buffers: Oxygen Geobarometers and Geothermometers
66(1)
Kinetics
66(6)
Activation Energy
67(1)
Overstepping and Metastable Persistence and Growth
68(4)
Silicate Melts and Volatile Fluids in Magma Systems
Nature of Magma
72(3)
Atomic Structure of Melts
73(2)
Volatile Fluids in Melts
75(5)
Nature of Volatiles
75(1)
Solubilities of Volatiles in Silicate Melts
76(3)
Exsolution of Volatiles from a Melt
79(1)
Consequences of Fluid Exsolution from Melts
80(7)
Explosive Volcanism
80(2)
Global Atmosphere and Climate
82(2)
Fumaroles, Hydrothermal Solutions, Ore Deposits, and Geothermal Reservoirs
84(3)
Crystal-Melt Equilibria in Magmatic Systems
Phase Diagrams
87(2)
Phase Rule
87(2)
Melting of a Pure Mineral and Polymorphism
89(1)
Volatile-Free Equilibria
89(1)
Melting of a Pure Mineral in the Presence of Volatiles
89(1)
Phase Relations in Binary Systems
90(8)
Basic Concepts: CaMgSi2O6 (Di)-CaAl2Si2O8 (An) System at P = 1 atm
90(3)
Mg2SiO4-SiO2 System at 1 atm
93(5)
Crystal-Melt Equilibria in Real Basalt Magmas
98(2)
Makaopuhi Basalt
98(1)
Basalt Magmas at High Pressures and High Water Concentrations
99(1)
Feldspar-Melt Equilibria
100(12)
KAlSi3O8 (Kf)-CaAl2Si2O8 (An) Binary System: Limited Solid Solution
100(1)
NaAlSi3O8 (Ab)-CaAl2Si2O8 (An) Binary Plagioclase System: Complete Solid Solution
101(1)
NaAlSi3O8 (Ab)-KAlSi3O8 (Kf) Binary Alkali Feldspar System
102(2)
KAlSi3O8 (Kf)-NaAlSi3O8 (Ab)-CaAl2Si2O8 (An) Ternary Feldspar System
104(4)
KAlSi3O8 (Kf)-NaAlSi3O8 (Ab)-SiO2 (silica)-H2O: The Granite System
108(4)
Crystal-Melt Equilibria Involving Anhydrous Mafic Minerals: Olivine and Pyroxene
112(1)
Crystal-Melt Equilibria in Hydrous Magma Systems
113(4)
Equilibria in the Granodiorite-Water System
113(1)
Equilibria Involving Melt and Micas and Amphiboles
114(3)
Geothermometers and Geobarometers
117(1)
Assessing States of Equilibrium in Rocks
117(1)
A Brief Comment Regarding Subsolidus Reactions in Magmatic Rocks
118(4)
Chemical Dynamics of Melts and Crystals
Viscosity of Melts
122(4)
Chemical Diffusion
126(4)
Types of Diffusion
126(1)
Theory and Measurement
127(1)
Factors Governing Diffusivities
128(1)
Average Diffusion Distance
129(1)
Soret Diffusion
129(1)
Diffusion of Heat
130(1)
The Role of Body Shape on Conductive Cooling
131(1)
Interfacial Energy
131(2)
Crystallization
133(6)
Why Is It Important to Study Nucleation and Crystallization?
133(1)
Nucleation
133(2)
Crystal Growth
135(2)
Crystal Size in Magmatic Rocks
137(2)
Secondary Overprinting Processes Modifying Primary Crystal Size and Shape
139(3)
Crystal Dissolution
139(1)
Textural Equilibration: Grain Boundary Modification
140(2)
Vesiculation and Fragmentation of Magma
142(9)
Nucleation and Growth of Bubbles---Vesiculation
142(3)
Melt Fragmentation and Explosive Volcanism
145(6)
Kinetic Paths and Fabric of Magmatic Rocks
Fabrics Related to Crystallization Path: Crystallinity and Grain Size
151(7)
Glassy Texture
151(2)
Aphanitic Texture
153(2)
Phaneritic Texture
155(2)
Porphyritic Texture
157(1)
Poikilitic and Ophitic Textures
158(1)
Fabrics Related to Crystallization Path: Grain Shape
158(2)
Fabrics Related to Crystallization Path: Inhomogeneous Grains
160(2)
Zoned Crystals
160(1)
Reaction Rims
160(1)
Subsolidus Decomposition and Exsolution in Unstable Minerals
161(1)
Fabric Related to Textural Equilibration: Secondary Grain-Boundary Modification
162(1)
A Word of Caution on the Interpretation of Crystalline Textures
163(2)
Magmatic Rock Texture and Order of Crystallization
163(2)
Fabrics Related to Nonexplosive Exsolution of Volatile Fluids
165(1)
Volcaniclastic Fabrics Related to Fragmentation of Magma
166(5)
Pyroclastic Processes
167(2)
Autoclastic Processes
169(2)
Fabrics Related to Consolidation of Volcaniclasts into Solid Rock
171(1)
Anisotropic Fabrics
171(10)
Descriptive Geometric Aspects
171(4)
Origin
175(6)
Inclusions
181(2)
Physical and Thermal Dynamics of Bodies of Magma
Stress and Deformation
183(3)
Concepts of Stress
183(1)
Deformation
184(1)
Ideal Response to Stress
185(1)
Rheology of Rocks and Magmas
186(8)
Rheology of Rocks
187(3)
Non-Newtonian Rheology of Magma
190(1)
Deformation and Flow of Magma
191(3)
Density of Magma and Buoyancy
194(3)
Density Determinations
194(1)
Densities of Minerals and Melts
195(1)
Buoyancy
196(1)
Conductive Heat Transfer
197(2)
Conductive Cooling Models
198(1)
Advective Heat Transfer
199(2)
Magma Convection
201(9)
Thermal Convection in a Completely Molten Body of Melt
201(2)
Thermochemical Convection in Crystallizing Magmas
203(2)
Replenishment in Evolving Magma Chambers
205(5)
Magma Ascent and Emplacement: Field Relations of Intrusions
Movement of Magma in the Earth
210(3)
Neutral Buoyancy and the Crustal Density Filter
210(2)
Magma Overpressure
212(1)
Mechanisms of Magma Ascent
213(1)
Sheet Intrusions (Dikes)
213(9)
Description and Terminology
213(3)
Some Thermomechanical Concepts Pertaining to Emplacement of Sheet Intrusions
216(2)
Geometry and Orientation of Sheet Intrusions
218(2)
Basalt Diking in Extensional Regimes
220(2)
Diapirs
222(2)
Magma Emplacement in the Crust: Providing the Space
224(17)
Some Aspects of Granitic Plutons
225(1)
Emplacement Processes and Factors
226(10)
The Intrusion--Host Rock Interface
236(5)
Magma Extrusion: Field Relations of Volcanic Rock Bodies
Overview of Extrusion: Controls and Factors
241(4)
Moving Magma to the Surface: What Allows Extrusion
242(1)
Two Types of Extrusions: Explosive and Effusive
242(3)
Effusions of Basaltic Lava
245(9)
Types of Basaltic Lava Flows
245(4)
Columnar Joints
249(1)
Subaerial Lava Accumulations
250(2)
Submarine Basaltic Accumulations
252(2)
Effusions of Silicic Lava
254(5)
Morphological Characteristics and Growth
254(2)
Internal Fabric
256(3)
Explosive Eruptions
259(19)
Explosive Mechanisms: Production of Pyroclasts
259(3)
Pyroclasts in Volcanic Plumes
262(1)
Pyroclast Transport and Deposition
262(5)
Explosive Style
267(3)
Pyroclastic Flows and Deposits: Overview
270(1)
Block-and-Ash Flows
271(1)
Ignimbrite-Forming Ash Flows
271(4)
Calderas
275(2)
Subaqueous Pyroclastic Flows
277(1)
Other Volcaniclastic Deposits
278(5)
Epiclastic Processes and Deposits
278(1)
Volcanic Debris Flows: Lahars
278(1)
Composite Volcanoes
279(4)
Generation of Magma
Melting of Solid Rock: Changes in P, T, and X
283(5)
Temperature Increase, +ΔT
284(2)
Decompression, -ΔP
286(1)
Changes in Water Concentration, +ΔXwater
287(1)
Mantle Source Rock
288(7)
Mantle-Derived Inclusions
289(2)
Metasomatized and Enriched Mantle Rock
291(4)
Generation of Magma in Mantle Peridotite
295(5)
Equilibrium (Batch) Partial Melting of Lherzolite
295(2)
Fractional Partial Melting of Lherzolite
297(1)
Factors Controlling Partial Melt Composition
297(2)
Modeling Partial Melting Using Trace Elements
299(1)
Characteristics of Primary Magma
300(1)
Magma Generation in Subarc Mantle Wedge
300(6)
Dehydration of Subducting Oceanic Crust
301(2)
Magma Generation in the Mantle Wedge
303(2)
Partial Melting of Subducted Basaltic Oceanic Crust: Adakite
305(1)
Generation of Alkaline Magmas in Metasomatically Enriched Mantle Peridotite
306(2)
The Metasomatized Mantle Connection
307(1)
Magma Generation in the Continental Crust
308(9)
Partial Melting of Continental Source Rocks
309(2)
``Alphabet'' Granitic Magmas: Contrasting Sources
311(1)
Crystalline Residues
312(1)
Melt Segregation
313(1)
Felsic Magma Generation and the Mantle Connection
313(4)
Differentiation of Magmas
Using Variation Diagrams to Characterize Differentiation Processes
317(1)
Closed-System Magmatic Differentiation
318(7)
Crystal-Melt Fractionation
318(4)
Physical Separation of Immiscible Melts
322(2)
Fluid-Melt Separation: Pegmatites
324(1)
Open-System Differentiation: Hybrid Magmas
325(4)
Magma Mixing
325(3)
Assimilation
328(1)
Differentiation in Basaltic Intrusions
329(9)
Palisades Sill
329(2)
Layered Intrusions
331(6)
Oceanic-Ridge Magma Chambers
337(1)
Origin of the Calc-Alkaline Differentiation Trend
338(11)
Tonga--Kermadec--New Zealand Arc
339(1)
Factors Controlling Development of the Calc-Alkaline Trend
339(10)
Magmatic Petrotectonic Associations
Oceanic Spreading Ridges and Related Basaltic Rocks
349(5)
Mid-Ocean Ridge Basalt (MORB)
350(3)
Iceland
353(1)
Mantle Reservoirs
354(1)
Mantle Plumes and Oceanic Island Volcanic Rocks
354(10)
Character of Volcanic Rocks
356(3)
Hawaiian Islands: Tholeiitic and Alkaline Associations
359(3)
Highly Alkaline Rocks on Other Oceanic Islands
362(2)
Plume Heads and Basalt Flood Plateau Lavas
364(6)
Oceanic Plateaus
364(1)
Continental Flood Basalt Plateaus
365(4)
Continental Breakup
369(1)
Arc Magmatism: Overview
370(1)
Oceanic Island Arcs
371(5)
Rock Associations
372(2)
Magma Evolution
374(1)
Back-Arc Basins
375(1)
Ophiolite
376(1)
Characteristics
376(1)
Origin and Emplacement
377(1)
Calc-Alkaline Continental Margin Magmatic Arcs
377(9)
Volcanic Arcs on Continental Margins
378(4)
Plutonic Arcs on Continental Margins: Granitic Batholiths
382(4)
Granites in Continent-Continent Collision Zones
386(1)
Anorogenic A-Type Felsic Rocks
387(3)
Characteristics
388(1)
Petrogenesis
389(1)
Anorogenic Ring Complexes in Nigeria and Niger
390(1)
Granites and Granites
390(2)
Continental Rift Associations: Bimodal and Alkaline Rocks
392(5)
Transitions from Continental Arc to Rift Associations in Western North America
394(1)
Magmatism in the East African Rift System
395(2)
Alkaline Orphans, Mostly in Stable Cratons
397(8)
Lamprophyres
398(1)
Lamproite, Orangeite, and Kimberlite Clans
398(7)
Metamorphic Rocks and Metamorphism: An Overview
Examples of Equilibration in Metamorphic Rocks
405(19)
Incipient Metamorphism: Crystallization of New Minerals and Preservation of Relict Protolith Fabrics
405(5)
Recrystallization under Hydrostatic Conditions: Newly Imposed Granoblastic Fabric
410(4)
Recrystallization under Nonhydrostatic States of Stress: Tectonite Fabric
414(7)
Crystalloblastic Series
421(1)
Metasomatism
422(2)
The Nature of Metamorphism
424(17)
The Nature of the Protolith
424(2)
Types of Metamorphism Based on Metamorphic Conditions
426(1)
Geologic Field Settings: Metamorphic Terranes
426(4)
Metamorphic Grade
430(1)
Metamorphic Zones
431(5)
Intensive Variables and Stable Mineral Assemblages
436(1)
Metamorphic Facies
437(1)
Metamorphic Facies Series
438(1)
Metamorphic Field Gradients and P--T--t Paths
438(3)
Why Study Metamorphic Rocks? Metamorphic Petrology and Continental Evolution and Tectonics
441(6)
Petrography of Metamorphic Rocks: Fabric, Composition, and Classification
Metamorphic Fabrics
447(8)
Anisotropic Fabrics of Tectonites
448(4)
Summary List of Metamorphic Textures
452(3)
Classification and Description of Metamorphic Rocks
455(11)
Metamorphic Rock Names Based on Fabric
455(1)
Strongly Foliated Rocks
456(1)
Weakly Foliated Rocks
457(3)
Nonfoliated Mafic Rocks
460(1)
Nonfoliated High-Grade Felsic Rocks
461(1)
Other Nonfoliated Metamorphic Rocks
462(1)
Serpentinite
463(2)
Metasomatic Rock Types
465(1)
Misfits
465(1)
High-Strain-Rate Rocks in Fault and Shear Zones
465(1)
Veins
466(1)
Graphical Representation of Mineral Assemblages in Composition Diagrams
466(8)
Fundamentals
466(1)
Examples of Composition Diagrams in Hypothetical Three-Component Systems
467(2)
Compatibility Diagrams for Metamorphic Rocks
469(5)
Metamorphic Mineral Reactions and Equilibria
Equilibrium Mineral Assemblages
474(1)
Overview of Metamorphic Mineral Reactions
475(1)
Polymorphic Transitions
475(4)
The Al2SiO5 System
476(3)
Net Transfer Solid--Solid Reactions
479(5)
Basic Relations in a System of Pure End-Member Phases
479(2)
Model Reactions in the Basalt--Granulite--Eclogite Transition
481(3)
Continuous Reactions Between Crystalline Solid Solutions
484(4)
Solid Solution in the Continuous Net Transfer Reaction Plagioclase = Jadeitic Clinopyroxene + Quartz
485(1)
Continuous Exchange Reactions in Fe--Mg Solid Solutions
485(3)
Solid--Fluid Mineral Reactions
488(10)
Fluids in the Crust of the Earth
488(3)
Fundamental Concepts of Solid--Fluid Reactions
491(2)
Equilibria with Mixed-Volatile Fluids
493(2)
Local versus External Control of Fluid Composition during Devolatilization Reactions
495(3)
Fluid Flow During Metamorphism of the Continental Crust
498(6)
Evidence for Fluid Flow
498(2)
Mechanics of Fluid Flow
500(4)
Metasomatism
504(4)
Ion Exchange Reactions in Open Metasomatic Systems
504(1)
The Thompson Model of Metasomatic Zoning and Local Equilibrium
505(1)
Low-Variance Assemblages in Metasomatic Rocks
506(1)
Frames of Reference and the Isocon Diagram
506(2)
Redox Mineral Equilibria
508(1)
Kinetics and Mineral Reactions: What Actually Happens in Metamorphic Rocks
509(2)
Role of Fluids in the Mechanism of Metamorphic Reactions
509(2)
Putting Mineral Equilibria to Work: Broader Petrologic Implications
511(10)
Isograds
511(2)
Evaluation of Intensive Variables during Metamorphism
513(1)
Mineral Thermobarometers
514(7)
Evolution of Imposed Metamorphic Fabrics: Processes and Kinetics
Solid-State Crystallization Under Static Conditions
521(7)
Nucleation and Growth
522(2)
Equilibration of Grain Size and Shape
524(2)
Intragrain Textural Features
526(2)
Ductile Flow
528(15)
Diffusive Creep
529(3)
Intracrystalline Plastic Deformation
532(6)
Crystal Defects
538(3)
Recovery during Dislocation Creep
541(1)
Hydrolytic Weakening of Silicates during Plastic Slip
541(2)
Power Law in Ductile Flow
543(1)
Interactions Between Deformation, Crystallization, and Fluids in Tectonites
543(12)
Role of Fluids in Tectonite Fabric Development
545(1)
Timing of Deformation and Crystallization: Larger Scale Implications
545(1)
Pre-, Syn-, and Postkinematic Fabrics
546(3)
Polymetamorphism
549(2)
Shear-Sense Indicators
551(3)
Patterns of Deformation and Flow: Tectonic Significance of Fabric Geometry
554(1)
Origin of Anisotropic Fabric in Metamorphic Tectonites
555(10)
Preferred Dimensional Orientation of Mineral Grains
556(1)
Preferred Orientation of Crystal Lattices in Tectonites
556(2)
Cleavage, Schistosity, and Compositional Layering
558(7)
Metamorphism at Convergent Plate Margins: P--T--t Paths, Facies, and Zones
P--T--t Paths
565(4)
Thermal Considerations
565(1)
Petrologic Determination of P--T--t Paths
566(3)
A Brief Anatomical Overview of Metamorphism in Orogens
569(7)
Specific Regional Metamorphic Terranes
570(6)
Intermediate- to Low-P Metamorphic Zones and Facies
576(13)
Pelitic Rocks in Typical Barrovian Zones at Intermediate Pressures
576(6)
P--T--t Paths and Chronology of Barrovian Metamorphism
582(1)
Buchan Metamorphism
583(4)
Mineral Assemblages in Mafic Protoliths: A Brief Overview
587(1)
Metabasites at Intermediate Pressures
587(2)
Ocean-Ridge Metamorphism
589(3)
Petrology of Metamorphosed Seafloor Rocks
590(2)
Intact Slabs of Ophiolite
592(2)
Near-Trench Metamorphic Associations
594(7)
The Franciscan Complex, California
594(1)
Melange
594(2)
Serpentinite
596(1)
Subgreenschist Facies Rocks
597(2)
Metabasites at High Pressures
599(1)
P--T--t Paths and Tectonic Evolution of High P/T Terranes
600(1)
Ultrahigh-P Metamorphic Rocks
601(11)
Coesite and Diamond: Diagnostic UHP Minerals
602(1)
Dora Maira Massif in the Western Alps
603(2)
Dabie--Sulu Terrane
605(1)
Evolution of UHP Terranes
606(6)
Precambrian Rock Associations
The Young Earth---A Brief Overview
612(1)
Archean Granitoid--Greenstone Terranes
613(10)
General Character of Greenstone Belts
614(3)
Itsaq Gneiss Complex, West Greenland: Earliest Record of Crustal Process at 3900--3600 Ma
617(3)
Kaapvaal Craton
620(1)
Yilgarn Craton
621(1)
Superior Province
622(1)
Archean Volcanic Rocks
623(10)
Komatiite
623(6)
Basalts
629(1)
Archean Megacrystic Anorthosite
630(2)
Other Volcanic Rocks in Greenstone Belts
632(1)
Archean Granitoids
633

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