Global tectonics.

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Bibliographic Details
Main Author: Kearey, P.
Other Authors: Klepeis, Keith A., Vine, F. J.
Language:English
Published: Oxford ; Chichester, West Sussex ; Hoboken, NJ : Wiley-Blackwell, 2009.
Edition:Third edition /
Subjects:
Genre:
Physical Description:xii, 482 pages, 16 unnumbered pages of plates : illustrations (some color), maps (some color) ; 25 cm
Format: Book
Contents:
  • 1 Historical perspective: 1.1 Continental drift
  • 1.2 Sea floor spreading and the birth of plate tectonics
  • 1.3 Geosynclinal theory
  • 1.4 Impact of plate tectonics. 2 The interior of the Earth: 2.1 Earthquake seismology
  • 2.1.1 Introduction
  • 2.1.2 Earthquake descriptors
  • 2.1.3 Seismic waves
  • 2.1.4 Earthquake location
  • 2.1.5 Mechanism of earthquakes
  • 2.1.6 Focal mechanism solutions of earthquakes
  • 2.1.7 Ambiguity in focal mechanism solutions
  • 2.1.8 Seismic tomography
  • 2.2 Velocity structure of the Earth
  • 2.3 Composition of the Earth
  • 2.4 The crust
  • 2.4.1 The continental crust
  • 2.4.2 Upper continental crust
  • 2.4.3 Middle and lower continental crust
  • 2.4.4 The oceanic crust
  • 2.4.5 Oceanic layer 1
  • 2.4.6 Oceanic layer 2
  • 2.4.7 Oceanic layer 3
  • 2.5 Ophiolites
  • 2.6 Metamorphism of oceanic crust
  • 2.7 Differences between continental and oceanic crust
  • 2.8 The mantle
  • 2.8.1 Introduction
  • 2.8.2 Seismic structure of the mantle
  • 2.8.3 Mantle composition
  • 2.8.4 The mantle low velocity zone
  • 2.8.5 The mantle transition zone
  • 2.8.6 The lower mantle
  • 2.9 The core
  • 2.10 Rheology of the crust and mantle
  • 2.10.1 Introduction
  • 2.10.2 Brittle deformation
  • 2.10.3 Ductile deformation
  • 2.10.4 Lithospheric strength profiles 2.10.5 Measuring continental deformation
  • 2.10.6 Deformation in the mantle
  • 2.11 Isostasy
  • 2.11.1 Introduction
  • 2.11.2 Airy's hypothesis
  • 2.11.3 Pratt's hypothesis
  • 2.11.4 Flexure of the lithosphere
  • 2.11.5 Isostatic rebound
  • 2.11.6 Tests of isostasy
  • 2.12 Lithosphere and asthenosphere
  • 2.13 Terrestrial heat flow. 3 Continental drift: 3.1 Introduction
  • 3.2 Continental reconstructions
  • 3.2.1 Euler's theorem
  • 3.2.2 Geometric reconstructions of continents
  • 3.2.3 The reconstruction of continents around the Atlantic
  • 3.2.4 The reconstruction of Gondwana
  • 3.3 Geologic evidence for continental drift
  • 3.4 Paleoclimatology
  • 3.5 Paleontologic evidence for continental drift
  • 3.6 Paleomagnetism
  • 3.6.1 Introduction
  • 3.6.2 Rock magnetism
  • 3.6.3 Natural remanent magnetization
  • 3.6.4 The past and present geomagnetic field
  • 3.6.5 Apparent polar wander curves
  • 3.6.6 Paleogeographic reconstructions based on paleomagnetism. 4 Sea floor spreading and transform faults: 4.1 Sea floor spreading
  • 4.1.1 Introduction
  • 4.1.2 Marine magnetic anomalies
  • 4.1.3 Geomagnetic reversals
  • 4.1.4 Sea floor spreading
  • 4.1.5 The Vine-Matthews hypothesis
  • 4.1.6 Magnetostratigraphy
  • 4.1.7 Dating of the ocean floor
  • 4.2 Transform faults
  • 4.2.1 Introduction
  • 4.2.2 Ridge-ridge transform faults
  • 4.2.3 Ridge jumps and transform fault offsets. 5 The framework of plate tectonics: 5.1 Plates and plate margins
  • 5.2 Distribution of earthquakes
  • 5.3 Relative plate motions
  • 5.4 Absolute plate motions
  • 5.5 Hotspots
  • 5.6 True polar wander
  • 5.7 Cretaceous superplume
  • 5.8 Direct measurement of relative plate motions
  • 5.9 Finite plate motions
  • 5.10 Stability of triple junctions
  • 5.11 Present day triple junctions. 6 Ocean ridges: 6.1 Ocean ridge topography
  • 6.2 Broad structure of the upper mantle below ridges
  • 6.3 Origin of anomalous upper mantle beneath ridges
  • 6.4 Depth-age relationship of oceanic lithosphere
  • 6.5 Heat flow and hydrothermal circulation
  • 6.6 Seismic evidence for an axial magma chamber
  • 6.7 Along-axis segmentation of oceanic ridges
  • 6.8 Petrology of ocean ridges
  • 6.9 Shallow structure of the axial region
  • 6.10 Origin of the oceanic crust
  • 6.11 Propagating rifts and microplates
  • 6.12 Oceanic fracture zones. 7 Continental rifts and rifted margins: 7.1 Introduction
  • 7.2 General characteristics of narrow rifts
  • 7.3 General characteristics of wide rifts
  • 7.4 Volcanic activity
  • 7.4.1 Large igneous provinces
  • 7.4.2 Petrogenesis of rift rocks
  • 7.4.3 Mantle upwelling beneath rifts
  • 7.5 Rift initiation
  • 7.6 Strain localization and delocalization processes
  • 7.6.1 Introduction
  • 7.6.2 Lithospheric stretching
  • 7.6.3 Buoyancy forces and lower crustal flow
  • 7.6.4 Lithospheric flexure
  • 7.6.5 Strain-induced weakening
  • 7.6.6 Rheological stratification of the lithosphere
  • 7.6.7 Magma-assisted rifting
  • 7.7 Rifted continental margins
  • 7.7.1 Volcanic margins
  • 7.7.2 Nonvolcanic margins
  • 7.7.3 The evolution of rifted margins
  • 7.8 Case studies: the transition from rift to rifted margin
  • 7.8.1 The East African Rift system
  • 7.8.2 The Woodlark Rift
  • 7.9 The Wilson cycle. 8 Continental transforms and strike-slip faults: 8.1 Introduction
  • 8.2 Fault styles and physiography
  • 8.3 The deep structure of continental transforms
  • 8.3.1 The Dead Sea Transform
  • 8.3.2 The San Andreas Fault
  • 8.3.3 The Alpine Fault
  • 8.4 Transform continental margins
  • 8.5 Continuous versus discontinuous deformation
  • 8.5.1 Introduction
  • 8.5.2 Relative plate motions and surface velocity fields
  • 8.5.3 Model sensitivities
  • 8.6 Strain localization and delocalization mechanisms
  • 8.6.1 Introduction
  • 8.6.2 Lithospheric heterogeneity
  • 8.6.3 Strain-softening feedbacks
  • 8.7 Measuring the strength of transforms. 9 Subduction zones: 9.1 Ocean trenches
  • 9.2 General morphology of island arc systems
  • 9.3 Gravity anomalies of subduction zones
  • 9.4 Structure of subduction zones from earthquakes
  • 9.5 Thermal structure of the downgoing slab
  • 9.6 Variations in subduction zone characteristics
  • 9.7 Accretionary prisms
  • 9.8 Volcanic and plutonic activity
  • 9.9 Metamorphism at convergent margins
  • 9.10 Backarc basins. 10 Orogenic belts: 10.1 Introduction
  • 10.2 Ocean-continent convergence
  • 10.2.1 Introduction
  • 10.2.2 Seismicity, plate motions and subduction geometry
  • 10.2.3 General geology of the central and southern Andes
  • 10.2.4 Deep structure of the central Andes
  • 10.2.5 Mechanisms of noncollisional orogenesis
  • 10.3 Compressional sedimentary basins
  • 10.3.1 Introduction
  • 10.3.2 Foreland basins
  • 10.3.3 Basin inversion
  • 10.3.4 Modes of shortening in foreland fold-thrust belts
  • 10.4 Continent-continent collision
  • 10.4.1 Introduction
  • 10.4.2 Relative plate motions and collisional history
  • 10.4.3 Surface velocity fields and seismicity
  • 10.4.4 General geology of the Himalayan-Tibetan Plateau
  • 10.4.5 Deep structure
  • 10.4.6 Mechanisms of continental collision
  • 10.5 Arc-continent collision
  • 10.6 Terrane accretion and continental growth
  • 10.6.1 Terrane analysis
  • 10.6.2 Structure of accretionary orogens
  • 10.6.3 Mechanisms of terrane accretion. 11 Precambrian tectonics and the supercontinent cycle: 11.1 Introduction
  • 11.2 Precambrian heat flow
  • 11.3 Archean tectonics
  • 11.3.1 General characteristics of cratonic mantle lithosphere
  • 11.3.2 General geology of Archean cratons
  • 11.3.3 The formation of Archean lithosphere
  • 11.3.4 Crustal structure
  • 11.3.5 Horizontal and vertical tectonics
  • 11.4 Proterozoic tectonics
  • 11.4.1 General geology of Proterozoic crust
  • 11.4.2 Continental growth and craton stabilization
  • 11.4.3 Proterozoic plate tectonics
  • 11.5 The supercontinent cycle
  • 11.5.1 Introduction
  • 11.5.2 Pre-Mesozoic reconstructions
  • 11.5.3 A Late Proterozoic supercontinent
  • 11.5.4 Earlier supercontinents
  • 11.5.5 Gondwana-Pangea assembly and dispersal. 12 The mechanism of plate tectonics: 12.1 Introduction
  • 12.2 Contracting Earth hypothesis
  • 12.3 Expanding Earth hypothesis
  • 12.3.1 Calculation of the ancient moment of inertia of the Earth
  • 12.3.2 Calculation of the ancient radius of the Earth
  • 12.4 Implications of heat flow
  • 12.5 Convection in the mantle
  • 12.5.1 The convection process
  • 12.5.2 Feasibility of mantle convection
  • 12.5.3 The vertical extent of convection
  • 12.6 The forces acting on plates
  • 12.7 Driving mechanism of plate tectonics
  • 12.7.1 Mantle drag mechanism
  • 12.7.2 Edge-force mechanism
  • 12.8 Evidence for convection in the mantle
  • 12.8.1 Introduction
  • 12.8.2 Seismic tomography
  • 12.8.3 Superswells
  • 12.8.4 The D" layer
  • 12.9 The nature of convection in the mantle
  • 12.10 Plumes
  • 12.11 The mechanism of the supercontinent cycle. 13 Implications of plate tectonics: 13.1 Environmental change
  • 13.1.1 Changes in sea level and sea water chemistry
  • 13.1.2 Changes in oceanic circulation and the Earth?s climate
  • 13.1.3 Land areas and climate
  • 13.2 Economic geology
  • 13.2.1 Introduction
  • 13.2.2 Autochthonous and allochthonous mineral deposits
  • 13.2.3 Deposits of sedimentary basins
  • 13.2.4 Deposits related to climate
  • 13.2.5 Geothermal power
  • 13.3 Natural hazards.