Earth Materials

Höfundur Cornelis Klein; Anthony Philpotts

Útgefandi Cambridge University Press

Snið ePub

Print ISBN 9781107155404

Útgáfa 2

Höfundarréttur 2016

7.190 kr.

Description

Efnisyfirlit

  • Cover
  • Half title
  • Frontispiece
  • Title page
  • Imprints page
  • Dedication
  • Contents
  • Preface
  • Coverage
  • Acknowledgments to First Edition
  • Acknowledgments to Second Edition
  • Chapter 1 Introduction
  • 1.1 Formation of Earth’s Chemical Elements in Supernovae
  • 1.2 Birth of the Solar System and Earth
  • 1.3 Accretion and Early History of the Earth
  • 1.4 Internal Structure of the Earth
  • 1.5 Cooling of the Planet and Plate Tectonics
  • 1.6 Plate Tectonics and the Formation of Rocks
  • 1.6.1 Divergent Plate Boundaries
  • 1.6.2 Convergent Plate Boundaries
  • 1.6.3 Transform Boundaries
  • 1.6.4 Mantle Plumes and Hot Spots
  • 1.7 Outline of Subsequent Chapters
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 2 Materials of the Solid Earth
  • 2.1 Definition of a Mineral
  • 2.1.1 Examples of Some Familiar Minerals
  • 2.2 How Are Minerals Classified?
  • 2.3 How Are Minerals Named?
  • 2.4 What Is a Crystal, and What Is the Crystalline State?
  • 2.5 What Is a Rock?
  • 2.6 How Do Rocks Form? Classification into Igneous, Sedimentary, and Metamorphic
  • 2.7 Examples of Some Familiar Rocks
  • 2.8 Plate Tectonics and the Generation of Rocks
  • 2.8.1 Midocean-ridge Rock Factory
  • 2.8.2 Convergent-plate-boundary Rock Factory
  • 2.8.3 Continental Divergent-plate-boundary Rock Factory (Rift Valley)
  • 2.8.4 Mantle Plume Hot-spot Rock Factory
  • 2.8.5 Passive-margin Rock Factories
  • 2.8.6 Epeiric-sea Rock Factories
  • 2.8.7 Metamorphic Rock Factories
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 3 How Are Minerals Identified?
  • 3.1 Habit
  • 3.2 State of Aggregation
  • 3.3 Color and Luster
  • 3.3.1 Reasons for Color
  • Play of Color
  • Chatoyancy, Labradorescence, and Asterism
  • Fluorescence
  • Streak
  • 3.4 Cleavage
  • 3.5 Hardness
  • 3.6 Specific Gravity (Relative Density)
  • 3.6.1 Specific Gravity and Atomic Structure
  • 3.7 Magnetism, Solubility in Acid, and Radioactivity
  • Magnetism
  • Solubility in HCl
  • Radioactivity
  • 3.8 Instrumental Methods for the Quantitative Characterization of Minerals
  • 3.8.1 X-Ray Powder Diffraction
  • 3.8.2 Electron Beam Techniques: Scanning Electron Microscopy, Electron Microprobe Analysis, and Transmission Electron Microscopy
  • Mineral Composition
  • Electron Microprobe
  • Transmission Electron Microscopy
  • Summary
  • Review Questions
  • Further Reading
  • Chapter 4 Fundamentals of Crystal Structures
  • 4.1 Naturally Occurring Chemical Elements
  • 4.2 Atomic and Ionic Radii
  • 4.3 What Factors Control the Packing of Ions (and Atoms) in Mineral Structures?
  • 4.4 Pauling’s Rules
  • Rule 1. The Coordination Principle
  • Rule 2. The Electrostatic Valency Principle
  • Rule 3. Sharing of Polyhedral Elements (I)
  • Rule 4. Sharing of Polyhedral Elements (II)
  • Rule 5. The Principle of Parsimony
  • 4.5 What Forces Hold Crystal Structures Together?
  • 4.5.1 Electronic Configuration of Atoms and Ions
  • 4.5.2 Chemical Bonding
  • Covalent Bonding
  • Ionic Bonding
  • Metallic Bonding
  • Van der Waals Bonding
  • 4.6 Atomic Substitutions
  • 4.6.1 Factors Responsible for the Extent of Atomic Substitution (Solid Solution)
  • The size of the atoms or ions:
  • The charge on the ions:
  • The temperature at which atomic substitution occurs.
  • The availability of the ions
  • 4.6.2 Types of Solid Solution
  • Substitutional solid solution.
  • Interstitial solid solution.
  • Omission solid solution
  • Summary
  • Review Questions
  • Further Reading
  • Chapter 5 Introduction to Crystallography
  • 5.1 Symmetry Elements and Operations
  • Mirrors
  • Rotation Axes
  • Center of Symmetry
  • Rotoinversion Axes
  • 5.2 Combinations of Symmetry Elements
  • 5.3 The Six Crystal Systems
  • 5.3.1 Crystallographic Axes
  • 5.3.2 Hermann–Mauguin Symmetry Notation
  • 5.3.3 Crystallographic Notation for Planes in Crystals
  • 5.3.4 Definition of Crystal Form
  • 5.3.5 Crystallographic Notation for Directions in Crystals
  • 5.4 Crystal Projections
  • 5.5 Seven of the Thirty-two Point Groups
  • 4/m3¯2/m
  • 6/m2/m2/m
  • 3¯2/m
  • 4/m2/m2/m
  • 2/m2/m2/m
  • 2/m
  • 5.6 Twins
  • 5.7 Some Aspects of Space Groups
  • Translation
  • Screw Axes
  • Glide Planes
  • 5.7.1 Space Groups
  • 5.8 Polymorphism
  • Summary
  • Review Questions
  • Further Reading
  • Chapter 6 Minerals and Rocks Observed under the Polarizing Optical Microscope
  • 6.1 Light and the Polarizing Microscope
  • The Components of the Petrographic Microscope
  • 6.2 Passage of Light through a Crystal: Refractive Index and Angle of Refraction
  • The Example of Apatite
  • 6.3 Passage of Polarized Light through Minerals
  • Looking at Anisotropic Minerals
  • 6.4 Accessory Plates and Determination of Fast and Slow Vibration Directions
  • 6.5 Extinction Positions and the Sign of Elongation
  • 6.6 Anomalous Interference Colors, Pleochroism, and Absorption
  • 6.7 Mineral Identification Chart
  • 6.8 Uniaxial Optical Indicatrix
  • The Example of Zircon
  • 6.9 Biaxial Optical Indicatrix
  • 6.10 Uniaxial Interference Figures
  • The Example of Quartz
  • 6.11 Determination of Optic Sign from Uniaxial Optic Axis Figure
  • 6.12 Biaxial Interference Figures, Optic Sign, and Optic Angle (2V)
  • The Example of Muscovite
  • 6.13 Modal Analysis
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 7 Igneous Rock-forming Minerals
  • 7.1 Common Chemical Elements in the Earth’s Crust and in Mineral and Rock Analyses
  • 7.2 Calculation of Mineral Formulas
  • 7.3 Triangular Diagrams
  • 7.4 Systematic Mineralogical Descriptions of Common Igneous Minerals
  • 7.5 Plagioclase Feldspar: NaAlSi3O8–CaAl2Si2O8albite(Ab)anorthite(An)
  • 7.6 K-Feldspar: KAlSi3O8 with Three Polymorphs (Microcline, Orthoclase, and Sanidine)
  • 7.7 Quartz: SiO2 and Polymorphs Tridymite, Cristobalite, Coesite, and Stishovite
  • 7.8 Nepheline: (Na,K)AlSiO4
  • 7.9 Leucite: KAlSi2O6
  • 7.10 Sodalite: Na4Al3Si3O12Cl
  • 7.11 Enstatite: MgSiO3−(Mg,Fe)SiO3
  • 7.12 Pigeonite: ~Ca0.25(Mg,Fe)1.75Si2O6
  • 7.13 Augite: (Ca,Na)(Mg,Fe,Al)(Si,Al)2O6
  • 7.14 Aegirine: NaFe3+Si2O6
  • 7.15 Hornblende: (Na,K)0−1Ca2(Mg,Fe,Al)5(Si,Al)8O22(OH)2
  • 7.16 Muscovite: KAl2(AlSi3O10)(OH)2
  • 7.17 Phlogopite: KMg3(AlSi3O10)(OH)2
  • 7.18 Biotite: K(Mg,Fe)3(AlSi3O10)(OH)2
  • 7.19 Olivine: (Mg,Fe)2SiO4
  • 7.20 Zircon: ZrSiO4
  • 7.21 Tourmaline: (Na,Ca,K)(Fe2+,Mg,Al,Mn,Li)3(Al,Fe3+)6(BO3)3(Si6O18)(OH)3(O,OH,F)
  • 7.22 Allanite: (Ca,Ce)2(Al,Fe2+,Fe3+)3(SiO4)(Si2O7)(OH)
  • 7.23 Melilite: (Ca,Na)2(Mg,Al)(Si,Al)2O7
  • 7.24 Magnetite: Fe3O4
  • 7.25 Chromite: FeCr2O4
  • 7.26 Hematite: Fe2O3
  • 7.27 Ilmenite: FeTiO3
  • 7.28 Rutile: TiO2
  • 7.29 Uraninite: UO2
  • 7.30 Pyrite: FeS2
  • 7.31 Pyrrhotite: Fe1-xS
  • 7.32 Chalcopyrite: CuFeS2
  • 7.33 Apatite: Ca5(PO4)3(OH,F,Cl)
  • Summary
  • Review Questions
  • Further Reading
  • Chapter 8 The Direction and Rate of Natural Processes: An Introduction to Thermodynamics and Kinetics
  • 8.1 Basic Thermodynamic Terms
  • System
  • Heat and Work
  • Variables
  • 8.2 Heat, Work, and the First Law of Thermodynamics
  • 8.3 Entropy and the Second and Third Laws of Thermodynamics
  • 8.4 Gibbs Free Energy
  • 8.5 Variation of Gibbs Free Energy with Temperature and Pressure
  • 8.6 Variation of Gibbs Free Energy with Composition
  • 8.7 Thermodynamic Equilibrium
  • 8.8 Thermodynamic Phase Diagrams
  • 8.9 Multicomponent Phase Diagrams
  • 8.9.1 A Simple Two-component System H2O–NaCl
  • 8.9.2 Melting of a Pair of Minerals: the Eutectic
  • Melting and Crystallization in a Simple Eutectic Phase Diagram
  • Igneous Textures Related to a Eutectic
  • 8.9.3 Congruent Melting and the Granite and Nepheline Syenite Eutectics
  • 8.9.4 Incongruent Melting and the Peritectic
  • 8.9.5 Melting Relations of Solid Solutions
  • Melting and Crystallizing Olivine
  • Melting and Crystallizing Plagioclase
  • Melting and Crystallizing Alkali Feldspars
  • 8.9.6 A Simple Ternary Phase Diagram
  • 8.9.7 The Ternary Quartz–Albite–Orthoclase “Granite” System
  • 8.9.8 A Simple Ternary Basalt System: Diopside–Albite–Anorthite
  • 8.9.9 More Complex Phase Diagrams
  • 8.10 Rates of Geologic Processes
  • 8.10.1 Transport Laws
  • 8.10.2 Rates of Activated Processes and the Arrhenius Relation
  • 8.11 Radioactive Decay
  • 8.11.1 Rate of Radioactive Decay
  • 8.11.2 Calculation of Absolute Age Based on Radioactive Decay
  • 8.11.3 Absolute Dating by the 87Rb to 87Sr Decay
  • 8.11.4 Absolute Dating by the 40K to 40Ar Decay
  • 8.11.5 Absolute Dating Using Uranium and Lead
  • 8.11.6 Absolute Dating by the 147Sm to 143Nd Decay
  • 8.11.7 Blocking Temperature
  • 8.11.8 Absolute Dating by the Fission-track Method
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 9 How Do Igneous Rocks Form?
  • 9.1 Why, and How, Does Solid Rock Become Molten?
  • 9.1.1 Composition of the Upper Mantle
  • 9.1.2 Melting Range of Upper Mantle Peridotite
  • 9.1.3 Latent Heat of Fusion
  • 9.1.4 Geothermal Gradient and the Geotherm
  • 9.2 Three Primary Causes of Melting and their Plate Tectonic Settings
  • 9.2.1 Raising the Temperature of Mantle Peridotite to the Melting Range over Hot Spots
  • 9.2.2 Decompression Melting at Divergent Plate Boundaries
  • 9.2.3 Fluxing with Water at Convergent Plate Boundaries (Subduction Zones)
  • 9.3 Effect of Pressure on Melting
  • 9.3.1 Pressure in the Earth
  • 9.3.2 Effect of Pressure on the Anhydrous Melting of Rock
  • 9.3.3 Hydrous Melting of Rock and the Solubility of Water in Magma
  • 9.3.4 Effect of Water Undersaturation on the Melting of Rocks
  • 9.3.5 Solubility of Other Gases in Magma
  • 9.3.6 Exsolution of Magmatic Gases and Explosive Volcanism
  • 9.4 Physical Properties of Magma
  • 9.4.1 Magma Density
  • 9.4.2 Magma Viscosity
  • 9.4.3 Diffusion in Magma, Crystal Growth, and Grain Size of Igneous Rocks
  • 9.5 Magma Ascent
  • 9.5.1 Buoyancy
  • 9.5.2 Buoyant Rise of Magma
  • 9.6 Processes Associated with the Solidification of Magma in the Crust
  • 9.6.1 Cooling of Bodies of Magma by Heat Conduction
  • Generalizations about the Cooling of Igneous Bodies
  • Effect of Latent Heat of Crystallization on Cooling of Magma
  • 9.6.2 Cooling of Bodies of Magma by Convection and Radiation
  • 9.6.3 Magmatic Differentiation by Crystal Settling
  • Igneous Cumulates
  • Igneous Layering
  • 9.6.4 Compaction of Crystal Mush
  • 9.6.5 Assimilation and Fractional Crystallization
  • Assimilation by Reaction
  • 9.6.6 Liquid Immiscibility
  • 9.7 Evolution of Isotopic Reservoirs in the Earth and the Source of Magma
  • 9.7.1 Evolution of 143Nd/144Nd Reservoirs in the Bulk Earth, Mantle, and Crust
  • 9.7.2 Evolution of 87Sr/86Sr Reservoirs in the Bulk Earth, Mantle, and Crust
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 10 Igneous Rocks
  • 10.1 Why an Igneous Rock Classification Is Necessary
  • 10.2 Mode of Occurrence of Igneous Rocks
  • 10.2.1 Shallow Intrusive Igneous Bodies: Dikes, Sills, Laccoliths, Cone Sheets, Ring Dikes, and Diatremes
  • Dikes, Sills, and Laccoliths
  • Cone Sheets and Ring Dikes
  • Diatremes
  • 10.2.2 Plutonic Igneous Bodies: Lopoliths, Batholiths, and Stocks
  • Lopoliths
  • Batholiths
  • Stocks
  • 10.2.3 Extrusive Igneous Bodies: Flood Basalts, Shield Volcanoes, Composite Volcanoes, Domes, Calderas, Ash-fall and Ash-flow Deposits
  • Flood Basalts
  • Shield Volcanoes
  • Composite Volcanoes
  • Domes
  • Calderas
  • Ash Falls and Ash Flows
  • 10.3 International Union of Geological Sciences Classification of Igneous Rocks
  • 10.3.1 Mode and Norm
  • 10.3.2 IUGS Classification of Igneous Rocks
  • 10.3.3 Composition of Common Plutonic Igneous Rocks
  • 10.3.4 IUGS Classification of Volcanic Igneous Rocks
  • 10.3.5 Irvine–Baragar Classification of Volcanic Rocks
  • 10.4 Igneous Rocks and their Plate Tectonic Setting
  • 10.4.1 Igneous Rocks Formed at Midocean-ridge Divergent Plate Boundaries
  • 10.4.2 Igneous Rocks of Oceanic Islands Formed above Hot Spots
  • 10.4.3 Continental Flood Basalts and Large Igneous Provinces
  • 10.4.4 Alkaline Igneous Rocks Associated with Continental Rift Valleys
  • 10.4.5 Igneous Rocks Formed near Convergent Plate Boundaries
  • Volcanic Arcs
  • Calcalkaline Magma Production above a Subducting Plate
  • Calcalkaline Volcanic Rocks
  • Calcalkaline Plutonic Rocks
  • 10.5 Special Precambrian Associations
  • 10.5.1 Komatiites
  • 10.5.2 Massif-type Anorthosites
  • 10.5.3 Rocks Associated with Large Meteorite Impacts
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 11 Sedimentary Rock-forming Minerals and Materials
  • 11.1 The Interaction of the Earth’s Atmosphere with Minerals
  • 11.2 Ice: H2O
  • 11.3 Goethite: FeO(OH)
  • 11.4 Kaolinite: Al2Si2O5(OH)4
  • 11.5 Calcite: CaCO3
  • 11.6 Aragonite: CaCO3
  • 11.7 Dolomite: CaMg(CO3)2
  • 11.8 Magnesite: MgCO3
  • 11.9 Siderite: FeCO3
  • 11.10 Rhodochrosite: MnCO3
  • 11.11 Halite: NaCl
  • 11.12 Sylvite: KCl
  • 11.13 Gypsum: CaSO4·2H2O
  • 11.14 Anhydrite: CaSO4
  • 11.15 Chert and Agate: Both Made of Very Fine-grained SiO2
  • 11.16 Phosphorite
  • 11.17 Soil
  • Summary
  • Review Questions
  • Further Reading
  • Chapter 12 Formation, Transport, and Lithification of Sediment
  • 12.1 Importance of Sediments in Understanding the History of the Earth
  • 12.2 Sediment Formed from Weathering of Rock
  • 12.2.1 Role of Carbon Dioxide in Weathering
  • 12.2.2 Weathering Products of Rock
  • 12.2.3 Detrital Grain Size
  • 12.2.4 Detrital Grain Roundness and Resistance to Abrasion
  • 12.3 Organically Produced Sediment
  • 12.3.1 Formation of Carbonate and Siliceous Sediment
  • Deepwater Calcareous and Siliceous Sediment
  • 12.3.2 Formation of Hydrocarbons in Sediment
  • 12.4 Chemically produced sediment
  • 12.5 Sediment Produced by Glacial Erosion
  • 12.6 Transport of Sediment
  • 12.6.1 Laminar and Turbulent Flow
  • 12.6.2 Movement of Particles by Fluid Flow
  • Rolling
  • Saltation
  • Suspension of Sedimentary Particles and Stokes’ Law
  • Bedforms
  • 12.6.3 Movement of particles in turbidity currents
  • 12.6.4 Movement of Sediment in Debris Flows
  • 12.7 Layering in Sediments and Sedimentary Rocks
  • 12.7.1 Law of Superposition
  • 12.7.2 Milankovitch Cycles
  • 12.7.3 Sediments Related to Tectonic Processes
  • Marine Transgressions and Regressions
  • 12.8 Sites of Deposition and Tectonic Significance
  • 12.8.1 Convergent Plate Boundaries
  • 12.8.2 Passive Continental Margins
  • 12.8.3 Rift and Pull-apart Basins
  • 12.9 Conversion of Unconsolidated Sediment to Sedimentary Rock: Lithification
  • 12.9.1 Porosity and compaction
  • 12.9.2 Cementation of Sediment
  • 12.9.3 Pressure Solution
  • 12.9.4 Recrystallization, Replacement, Dolomitization
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 13 Sedimentary Rock Classification, Occurrence, and Plate Tectonic Significance
  • 13.1 Siliciclastic Sedimentary Rocks
  • 13.1.1 Mudrocks (Includes Shales)
  • Tectonic Setting for Deposition of Mudrocks
  • 13.1.2 Sandstones
  • Quartz Arenites
  • Feldspathic Arenites (Arkose)
  • Lithic Arenites
  • Wackes (Graywacke)
  • 13.1.3 Conglomerates and Breccias
  • 13.2 Carbonate Sedimentary Rocks
  • 13.2.1 Limestones
  • Grainstone
  • Mudstones to Packstones
  • Boundstones
  • Lacustrine Limestones
  • Tufa, Travertine, and Caliche
  • 13.2.2 Dolostones
  • 13.2.3 Tectonic Settings of Carbonate Rocks
  • 13.3 Coals
  • 13.4 Oil and Natural Gas
  • 13.5 Evaporites
  • 13.6 Phosphorites
  • 13.7 Iron-formations
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 14 Metamorphic Rock-forming Minerals
  • 14.1 Systematic Mineralogical Descriptions of Common Metamorphic Minerals
  • 14.2 Garnet: (Mg2+,Fe2+,Mn2+)3Al2Si3O12 and Ca3(Fe3+,Al3+,Cr3+)2Si3O12
  • 14.3 Andalusite: Al2SiO5
  • 14.4 Sillimanite: Al2SiO5
  • 14.5 Kyanite: Al2SiO5
  • 14.6 Staurolite: Fe3−4Al18Si8O48H2−4
  • 14.7 Diopside: CaMgSi2O6
  • 14.8 Anthophyllite: Mg7Si8O22(OH)2
  • 14.9 Cummingtonite–Grunerite: Fe2Mg5Si8O22(OH)2−Fe7Si8O22(OH)2
  • 14.10 Tremolite–Ferroactinolite: Ca2Mg5Si8O22(OH)2−Ca2Fe5Si8O22(OH)2
  • 14.11 Glaucophane: Na2Mg3Al2Si8O22(OH)2
  • 14.12 Wollastonite: CaSiO3
  • 14.13 Rhodonite: MnSiO3
  • 14.14 Talc: Mg3Si4O10(OH)2
  • 14.15 Chlorite: (Mg, Al, Fe)6(Si, Al)4O10·(OH)8
  • 14.16 Antigorite: Mg3Si2O5(OH)4
  • 14.17 Chrysotile: Mg3Si2O5(OH)4
  • 14.18 Graphite: C
  • 14.19 Epidote: Ca2Fe3+Al2O(SiO4)(Si2O7)(OH) Clinozoisite: Ca2Al3O(SiO4)(Si2O7)(OH)
  • 14.20 Cordierite: (Mg,Fe)2Al4Si5O18·nH2O
  • 14.21 Vesuvianite: Ca19(Al,Mg,Fe)13(Si2O7)4(SiO4)10(O,OH,F)10
  • 14.22 Titanite (sphene): CaTiSiO5
  • 14.23 Scapolite: 3NaAlSi3O8·NaCl−3CaAl2Si2O8·CaSO4 (or ·CaCO3)
  • 14.24 Lawsonite: CaAl2(Si2O7)(OH)2·H2O
  • 14.25 Pumpellyite: Ca2MgAl2(SiO4)(Si2O7)(OH)2·H2O
  • 14.26 Topaz: Al2SiO4(F,OH)2
  • 14.27 Corundum: Al2O3
  • 14.28 Chabazite: Ca2Al2Si4O12·6H2O
  • Summary
  • Review Questions
  • Further Reading
  • Chapter 15 Metamorphic Rocks
  • 15.1 What Changes Occur during Metamorphism?
  • 15.1.1 An Example of Metamorphic Change
  • 15.2 Why Do Rocks Change?
  • 15.2.1 The Gibbs Free Energy, the Driving Force for Metamorphic Change
  • 15.2.2 Rates of Metamorphic Reactions
  • 15.2.3 The Gibbs Phase Rule and the Number of Minerals a Metamorphic Rock Can Contain
  • 15.3 Metamorphic Grade and Facies
  • 15.4 Textures of Metamorphic Rocks
  • 15.4.1 Textures of Contact Metamorphic Rocks
  • 15.4.2 Deformation and Textures of Regional Metamorphic Rocks
  • Slate, Phyllite, Schist, and Gneiss
  • Migration of Material during the Development of Foliation
  • Growth of Metamorphic Minerals during Shear
  • 15.5 Simple Descriptive Classification of Metamorphic Rocks
  • 15.6 Metamorphism of Mudrock
  • 15.6.1 Graphical Representation of a Simple Metamorphic Reaction
  • 15.6.2 A Simple Pressure–Temperature Petrogenetic Grid
  • 15.6.3 Metamorphic Field Gradients
  • 15.6.4 Graphical Representation of Mineral Assemblages in Metapelites
  • 15.6.5 Mineral Assemblages in Barrow’s Metamorphic Zones and Part of the Petrogenetic Grid for Metapelites
  • 15.7 Metamorphism of Impure Dolomitic Limestone
  • 15.8 Metamorphism and Partial Melting: Migmatites
  • 15.9 Geothermometers and Geobarometers
  • 15.10 Plate Tectonic Significance of Metamorphism
  • 15.10.1 Pressure–Temperature–time (P–T–t) paths
  • 15.10.2 Plate Tectonic Setting of Metamorphic Facies
  • Midocean Ridges
  • Convergent Plate Boundaries
  • Rifting and Delamination of Continental Crust
  • Overview of Metamorphism and Plate Tectonics
  • Summary
  • Review Questions
  • Further Reading
  • Chapter 16 Some Economic Minerals, Mainly from Veins and Pegmatites
  • 16.1 Gold: Au
  • 16.2 Silver: Ag
  • 16.3 Copper: Cu
  • 16.4 Diamond: C
  • 16.5 Sulfur: S
  • 16.6 Galena: PbS
  • 16.7 Sphalerite: ZnS
  • 16.8 Bornite: Cu5FeS4
  • 16.9 Chalcocite: Cu2S
  • 16.10 Marcasite: FeS2
  • 16.11 Molybdenite: MoS2
  • 16.12 Arsenopyrite: FeAsS
  • 16.13 Bauxite: a Mixture of Diaspore, Gibbsite, and Boehmite
  • 16.14 Fluorite: CaF2
  • 16.15 Barite: BaSO4
  • 16.16 Spodumene: LiAlSi2O6
  • 16.17 Lepidolite: K(Li,Al)2−3(AlSi3O10)(OH,F)2
  • 16.18 Several Gem Minerals
  • Ruby and Sapphire (Gem Varieties of Corundum, Al2O3)
  • Topaz
  • Tourmaline
  • Emerald, Heliodor, and Aquamarine (Gem Varieties of Beryl, Be3Al2Si6O18)
  • Opal
  • Jade
  • Turquoise
  • Summary
  • Review Questions
  • Further Reading
  • Chapter 17 Some Selected Earth Materials Resources
  • 17.1 Construction Materials
  • 17.1.1 Building Stones
  • 17.1.2 Bricks, Cement, and Concrete
  • 17.1.3 Crushed Stone, Sand, and Gravel
  • 17.2 Iron Ore
  • 17.3 Clay Minerals
  • 17.4 Copper Ore
  • 17.5 Lithium Ore
  • 17.6 Rare Earth Elements (REEs)
  • 17.7 Zeolites
  • 17.8 Energy Resources
  • 17.8.1 Oil, Natural Gas, and Coal Reserves
  • 17.8.2 Shale Gas and Hydraulic Fracturing
  • 17.8.3 Nuclear Energy
  • 17.8.4 Geothermal Energy
  • Summary
  • Review Questions
  • Online Resources
  • Further Reading
  • Chapter 18 Earth Materials and Human Health
  • 18.1 The Human Body’s Need for Earth Materials
  • 18.2 Soils and Human Health
  • 18.2.1 What Constitutes a Fertile Soil?
  • Volcanic Soils
  • Soil from Young Tectonic Regions
  • Glacial Soil
  • Wind-blown Soil (Loess)
  • 18.2.2 Increasing Crop Production from Agricultural Land, and Soil Depletion
  • 18.2.3 The Need for Fertilizers
  • 18.3 Carcinogenic and Chemical Hazards Posed by Earth Materials
  • 18.3.1 Erionite
  • 18.3.2 Asbestos Minerals
  • 18.3.3 Silica Minerals
  • 18.3.4 Arsenic, an Example of a Chemically Hazardous Earth Material
  • Arsenic in the General Environment
  • Arsenic in Groundwater in Southeast Asia
  • 18.3.5 Health Hazards Due to Radioactivity
  • Radon Gas
  • Radioactive Waste Disposal from Nuclear Power Plants
  • 18.3.6 Carbon Sequestration to Mitigate Climate Change
  • 18.4 Hazards from Volcanic Eruptions
  • 18.4.1 Monitoring Active Volcanoes
  • 18.4.2 Lahars
  • 18.5 Tsunamis
  • 18.6 Ejecta from Meteorite Impacts
  • Summary
  • Review Questions
  • Online Resources
  • USGS health and environment
  • Arsenic
  • Acid mine drainage
  • Carbon dioxide
  • Further Reading
  • Glossary
  • Minerals and Varieties
  • Common Igneous, Sedimentary, and Metamorphic Rocks
  • Common Units of Measure
  • Other Quantitative Terms
  • Index
  • Plates

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