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Global Tectonics

ISBN: 9781405107778 | 1405107774
Edition: 3rd
Format: Paperback
Publisher: Wiley-Blackwell
Pub. Date: 1/20/2009

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SummaryTable of ContentsAuthor Biography
The third edition of this widely acclaimed textbook provides a comprehensive introduction to all aspects of global tectonics. Revisions to this new edition reflect the most significant recent advances in the field, providing a thorough, accessible, and up-to-date text. Combining a historical approach with process science, Global Tectonics provides a careful balance between geological and geophysical material in both continental and oceanic regimes. New and expanded chapters in this third edition include Precambrian tectonics and the supercontin... MORE
Preface
Acknowledgments
Historical perspective
Continental drift
Sea floor spreading and the birth of plate tectonics
Geosynclinal theory
Impact of plate tectonics
The interior of the Earth
Earthquake seismology
Introduction
Earthquake descriptors
S... MORE
Earthquake location
Mechanism of earthquakes
Focal mechanism solutions of earthquakes
Ambiguity in focal mechanism solutions
Seismic tomography
Velocity structure of the Earth
Composition of the Earth
The crust
The continental crust
Upper continental crust
Middle and lower continental crust
The oceanic crust
Oceanic layer
Oceanic layer
Oceanic layer
Ophiolites
Metamorphism of oceanic crust
Differences between continental and oceanic crust
The mantle
Introduction
Seismic structure of the mantle
Mantle composition
The mantle low velocity zone
The mantle transition zone
The lower mantle
The core
Rheology of the crust and mantle
Introduction
Brittle deformation
Ductile deformation
Lithospheric strength profiles
Measuring continental deformation
Deformation in the mantle
Isostasy
Introduction
Airy's hypothesis
Pratt's hypothesis
Flexure of the lithosphere
Isostatic rebound
Tests of isostasy
Lithosphere and asthenosphere
Terrestrial heat flow
Continental drift
Introduction
Continental reconstructions
Euler's theorem
Geometric reconstructions of continents
The reconstruction of continents around the Atlantic
The reconstruction of Gondwana
Geologic evidence for continental drift
Paleoclimatology
Paleontologic evidence for continental drift
Paleomagnetism
Introduction
Rock magnetism
Natural remanent magnetization
The past and present geomagnetic field
Apparent polar wander curves
Paleogeographic reconstructions based on paleomagnetism
Sea floor spreading and transform faults
Sea floor spreading
Introduction
Marine magnetic anomalies
Geomagnetic reversals
Sea floor spreading
The Vine-Matthews hypothesis
Magnetostratigraphy
Dating of the ocean floor
Transform faults
Introduction
Ridge-ridge transform faults
Ridge jumps and transform fault offsets
The framework of plate tectonics
Plates and plate margins
Distribution of earthquakes
Relative plate motions
Absolute plate motions
Hotspots
True polar wander
Cretaceous superplume
Direct measurement of relative plate motions
Finite plate motions
Stability of triple junctions
Pre
Table of Contents provided by Publisher. All Rights Reserved.
Phil Kearey was Senior Lecturer in Applied Geophysics in the Department of Earth Sciences at Bristol University, U.K. prior to his premature death in 2003. In his research he used various types of geophysical data, but gravity and magnetic data in particular, to elucidate crustal structure in the eastern Caribbean, Canadian shield and southern England.

Keith Klepeis is an Associate Professor in the Department of Geology at the University of Vermont, U.S.A. He specializes in the areas of structural geology and continental tectonics and has worked extensively on the evolution of orogenic belts and fault systems in New Zealand, Patagonia, West Antarctica, Australia, British Columbia and southeast Alaska.

Fred Vine is an Emeritus Professor in the School of Environmental Sciences at the University of East Anglia, Norwich, U.K. He was made a Fellow of the Royal Society of London and has received numerous awards for work on the interpretation of oceanic magnetic anomalies and ophiolites, fragments of oceanic crust thrust up on land, in terms of sea floor spreading.


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