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0521859026 cambridge university press fundamentals of geophysics oct 2007

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  • Cover

  • Half-title

  • Title

  • Copyright

  • Contents

  • Preface to the second edition

  • Acknowledgements

  • 1 The Earth as a planet

    • 1.1 THE SOLAR SYSTEM

      • 1.1.1 The discovery and description of the planets

      • 1.1.2 Kepler’s laws of planetary motion

      • 1.1.3 Characteristics of the planets

        • 1.1.3.1 Bode’s law

        • 1.1.3.2 The terrestrial planets and the Moon

        • 1.1.3.3 The great planets

        • 1.1.3.4 Pluto and the outer solar system

        • 1.1.3.5 Angular momentum

      • 1.1.4 The origin of the solar system

    • 1.2 THE DYNAMIC EARTH

      • 1.2.1 Historical introduction

      • 1.2.2 Continental drift

        • 1.2.2.1 Pangaea

        • 1.2.2.2 Computer-assisted reconstructions

        • 1.2.2.3 Paleomagnetism and continental drift

      • 1.2.3 Earth structure

        • 1.2.3.1 Lithospheric plates

      • 1.2.4 Types of plate margin

      • 1.2.5 Sea-floor spreading

        • 1.2.5.1 The Vine–Matthews–Morley hypothesis

        • 1.2.5.2 Rates of sea-floor spreading

      • 1.2.6 Plate margins

        • 1.2.6.1 Constructive margins

        • 1.2.6.2 Destructive margins

        • 1.2.6.3 Conservative margins

      • 1.2.7 Triple junctions

        • 1.2.7.1 Stability of triple junctions

        • 1.2.7.2 Evolution of triple junctions in the northeast Pacific

      • 1.2.8 Hotspots

      • 1.2.9 Plate motion on the surface of a sphere

        • 1.2.9.1 Euler poles of rotation

        • 1.2.9.2 Absolute plate motions

      • 1.2.10 Forces driving plate tectonic motions

        • 1.2.10.1 Forces acting on lithospheric plates

        • 1.2.10.2 Relative magnitudes of forces driving plate motions

    • 1.3 SUGGESTIONS FOR FURTHER READING

      • Introductory level

      • Intermediate level

      • Advanced level

    • 1.4 REVIEW QUESTIONS

    • 1.5 EXERCISES

  • 2 Gravity, the figure of the Earth and geodynamics

    • 2.1 THE EARTH’S SIZE AND SHAPE

      • 2.1.1 Earth’s size

      • 2.1.2 Earth’s shape

    • 2.2 GRAVITATION

      • 2.2.1 The law of universal gravitation

        • 2.2.1.1 Potential energy and work

      • 2.2.2 Gravitational acceleration

        • 2.2.2.1 Gravitational potential

        • 2.2.2.2 Acceleration and potential of a distribution of mass

        • 2.2.2.3 Mass and mean density of the Earth

      • 2.2.3 The equipotential surface

    • 2.3 THE EARTH’S ROTATION

      • 2.3.1 Introduction

      • 2.3.2 Centripetal and centrifugal acceleration

        • 2.3.2.1 Centripetal acceleration

        • 2.3.2.2 Centrifugal acceleration and potential

        • 2.3.2.3 Kepler’s third law of planetary motion

        • 2.3.2.4 Verification of the inverse square law of gravitation

      • 2.3.3 The tides

        • 2.3.3.1 Lunar tidal periodicity

        • 2.3.3.2 Tidal effect of the Sun

        • 2.3.3.3 Spring and neap tides

        • 2.3.3.4 Effect of the tides on gravity measurements

        • 2.3.3.5 Bodily Earth-tides

      • 2.3.4 Changes in Earth’s rotation

        • 2.3.4.1 Effect of lunar tidal friction on the length of the day

        • 2.3.4.2 Increase of the Earth–Moon distance

        • 2.3.4.3 The Chandler wobble

        • 2.3.4.4 Precession and nutation of the rotation axis

        • 2.3.4.5 Milankovitch climatic cycles

      • 2.3.5 Coriolis and Eötvös accelerations

    • 2.4 THE EARTH’S FIGURE AND GRAVITY

      • 2.4.1 The figure of the Earth

      • 2.4.2 Gravitational potential of the spheroidal Earth

      • 2.4.3 Gravity and its potential

      • 2.4.4 Normal gravity

      • 2.4.5 The geoid

        • 2.4.5.1 Geoid undulations

      • 2.4.6 Satellite geodesy

        • 2.4.6.1 Satellite laser-ranging

        • 2.4.6.2 Satellite altimetry

        • 2.4.6.3 Satellite-based global positioning systems (GPS)

        • 2.4.6.4 Measurement of gravity and the geoid from orbiting satellites

        • 2.4.6.5 Observation of crustal deformation with satelliteborne radar

        • 2.4.6.6 Very long baseline interferometry

    • 2.5 GRAVITY ANOMALIES

      • 2.5.1 Introduction

      • 2.5.2 Absolute measurement of gravity

        • 2.5.2.1 Free-fall method

        • 2.5.2.2 Rise-and-fall method

      • 2.5.3 Relative measurement of gravity: the gravimeter

        • 2.5.3.1 Gravity surveying

      • 2.5.4 Correction of gravity measurements

        • 2.5.4.1 Latitude correction

        • 2.5.4.2 Terrain corrections

        • 2.5.4.3 Bouguer plate correction

        • 2.5.4.4 Free-air correction

        • 2.5.4.5 Combined elevation correction

      • 2.5.5 Density determination

        • 2.5.5.1 Density from seismic velocities

        • 2.5.5.2 Gamma–gamma logging

        • 2.5.5.3 Borehole gravimetry

        • 2.5.5.4 Nettleton’s method for near-surface density

      • 2.5.6 Free-air and Bouguer gravity anomalies

    • 2.6 INTERPRETATION OF GRAVITY ANOMALIES

      • 2.6.1 Regional and residual anomalies

      • 2.6.2 Separation of regional and residual anomalies

        • 2.6.2.1 Visual analysis

        • 2.6.2.2 Polynomial representation

        • 2.6.2.3 Representation by Fourier series

        • 2.6.2.4 Anomaly enhancement and filtering

      • 2.6.3 Modelling gravity anomalies

        • 2.6.3.1 Uniform sphere: model for a diapir

        • 2.6.3.2 Horizontal line element

        • 2.6.3.3 Horizontal cylinder: model for anticline or syncline

        • 2.6.3.4 Horizontal thin sheet

        • 2.6.3.5 Horizontal slab: model for a vertical fault

        • 2.6.3.6 Iterative modelling

      • 2.6.4 Some important regional gravity anomalies

        • 2.6.4.1 Continental and oceanic gravity anomalies

        • 2.6.4.2 Gravity anomalies across mountain chains

        • 2.6.4.3 Gravity anomalies across an oceanic ridge

        • 2.6.4.4 Gravity anomalies at subduction zones

    • 2.7 ISOSTASY

      • 2.7.1 The discovery of isostasy

      • 2.7.2 Models of isostasy

        • 2.7.2.1 The Airy–Heiskanen model

        • 2.7.2.2 The Pratt–Hayford model

        • 2.7.2.3 Vening Meinesz elastic plate model

      • 2.7.3 Isostatic compensation and vertical crustal movements

      • 2.7.4 Isostatic gravity anomalies

    • 2.8 RHEOLOGY

      • 2.8.1 Brittle and ductile deformation

      • 2.8.2 Viscous flow in liquids

      • 2.8.3 Flow in solids

        • 2.8.3.1 Viscoelastic model

      • 2.8.4 Creep

        • 2.8.4.1 Crystal defects

        • 2.8.4.2 Creep mechanisms in the Earth

      • 2.8.5 Rigidity of the lithosphere

        • 2.8.5.1 Lithospheric flexure caused by oceanic islands

        • 2.8.5.2 Lithospheric flexure at a subduction zone

        • 2.8.5.3 Thickness of the lithosphere

      • 2.8.6 Mantle viscosity

        • 2.8.6.1 Viscosity of the upper mantle

        • 2.8.6.2 Viscosity of the lower mantle

    • 2.9 SUGGESTIONS FOR FURTHER READING

      • Introductory level

      • Intermediate level

      • Advanced level

    • 2.10 REVIEW QUESTIONS

    • 2.11 EXERCISES

  • 3 Seismology and the internal structure of the Earth

    • 3.1 INTRODUCTION

    • 3.2 ELASTICITY THEORY

      • 3.2.1 Elastic, anelastic and plastic behavior of materials

      • 3.2.2 The stress matrix

      • 3.2.3 The strain matrix

        • 3.2.3.1 Longitudinal strain

        • 3.2.3.2 Dilatation

        • 3.2.3.3 Shear strain

      • 3.2.4 The elastic constants

        • 3.2.4.1 Bulk modulus in terms of Young’s modulus and Poisson’s ratio

        • 3.2.4.2 Shear modulus in terms of Young’s modulus and Poisson’s ratio

        • 3.2.4.3 The Lamé constants

        • 3.2.4.4 Anisotropy

      • 3.2.5 Imperfect elasticity in the Earth

    • 3.3 SEISMIC WAVES

      • 3.3.1 Introduction

      • 3.3.2 Seismic body waves

        • 3.3.2.1 Compressional waves

        • 3.3.2.2 Transverse waves

        • 3.3.2.3 The solution of the seismic wave equation

        • 3.3.2.4 D’Alembert’s principle

        • 3.3.2.5 The eikonal equation

        • 3.3.2.6 The energy in a seismic disturbance

        • 3.3.2.7 Attenuation of seismic waves

      • 3.3.3 Seismic surface waves

        • 3.3.3.1 Rayleigh waves (LR )

        • 3.3.3.2 Love waves (LQ)

        • 3.3.3.3 The dispersion of surface waves

      • 3.3.4 Free oscillations of the Earth

        • 3.3.4.1 Radial oscillations

        • 3.3.4.2 Spheroidal oscillations

        • 3.3.4.3 Toroidal oscillations

        • 3.3.4.4 Comparison with surface waves

    • 3.4 THE SEISMOGRAPH

      • 3.4.1 Introduction

      • 3.4.2 Principle of the seismometer

        • 3.4.2.1 Vertical-motion seismometer

        • 3.4.2.2 Horizontal-motion seismometer

        • 3.4.2.3 Strain seismometer

      • 3.4.3 The equation of the seismometer

        • 3.4.3.1 Effect of instrumental damping

        • 3.4.3.2 Long-period and short-period seismometers

        • 3.4.3.3 Broadband seismometers

      • 3.4.4 The seismogram

        • 3.4.4.1 Analog recording

        • 3.4.4.2 Digital recording

        • 3.4.4.3 Phases on a seismogram

    • 3.5 EARTHQUAKE SEISMOLOGY

      • 3.5.1 Introduction

      • 3.5.2 Location of the epicenter of an earthquake

      • 3.5.3 Global seismicity

      • 3.5.4 Analysis of earthquake focal mechanisms

        • 3.5.4.1 Single-couple and double-couple radiation patterns

        • 3.5.4.2 Fault-plane solutions

        • 3.5.4.3 Mechanics of faulting

        • 3.5.4.4 Focal mechanisms at active plate margins

        • 3.5.4.5 Focal mechanisms in continental collisional zones

      • 3.5.5 Secondary effects of earthquakes: landslides, tsunami, fires and fatalities

      • 3.5.6 Earthquake size

        • 3.5.6.1 Earthquake intensity

        • 3.5.6.2 Earthquake magnitude

        • 3.5.6.3 Relationship between magnitude and intensity

      • 3.5.7 Earthquake frequency

      • 3.5.8 Energy released in an earthquake

      • 3.5.9 Earthquake prediction

        • 3.5.9.1 Prediction of the location of an earthquake

        • 3.5.9.2 Prediction of the time and size of an earthquake

      • 3.5.10 Earthquake control

      • 3.5.11 Monitoring nuclear explosions

    • 3.6 SEISMIC WAVE PROPAGATION

      • 3.6.1 Introduction

      • 3.6.2 Huygens’ principle

        • 3.6.2.1 The law of reflection using Huygens’ principle

        • 3.6.2.2 The law of refraction using Huygens’ principle

        • 3.6.2.3 Diffraction

      • 3.6.3 Fermat’s principle

        • 3.6.3.1 The law of reflection using Fermat’s principle

        • 3.6.3.2 The law of refraction using Fermat’s principle

      • 3.6.4 Partitioning of seismic body waves at a boundary

        • 3.6.4.1 Subcritical and supercritical reflections, and critical refraction

      • 3.6.5 Reflection seismology

        • 3.6.5.1 Reflection at a horizontal interface

        • 3.6.5.2 Reflection at an inclined interface

        • 3.6.5.3 Reflection and transmission coefficients

        • 3.6.5.4 Synthetic seismograms

        • 3.6.5.5 Seismic noise

        • 3.6.5.6 Reflection seismic section

      • 3.6.6 Refraction seismology

        • 3.6.6.1 Refraction at a horizontal interface

        • 3.6.6.2 Refraction at an inclined interface

        • 3.6.6.3 Refraction with continuous change of velocity with depth

    • 3.7 INTERNAL STRUCTURE OF THE EARTH

      • 3.7.1 Introduction

      • 3.7.2 Refractions and reflections in the Earth’s interior

        • 3.7.2.1 Seismic rays in a uniformly layered Earth

        • 3.7.2.2 Travel-time curves for P-, PKP- and PKIKP-waves

      • 3.7.3 Radial variations of seismic velocities

        • 3.7.3.1 Inversion of travel-time versus distance curves

        • 3.7.3.2 Forward modelling: polynomial parametrization

      • 3.7.4 Radial variations of density, gravity and pressure

        • 3.7.4.1 Density inside the Earth

        • 3.7.4.2 Gravity and pressure inside the Earth

      • 3.7.5 Models of the Earth’s internal structure

        • 3.7.5.1 The crust

        • 3.7.5.2 The upper mantle

        • 3.7.5.3 The lower mantle

        • 3.7.5.4 The core

      • 3.7.6 Seismic tomography

        • 3.7.6.1 Travel-time residuals and velocity anomalies

        • 3.7.6.2 Mantle tomography

    • 3.8 SUGGESTIONS FOR FURTHER READING

      • Introductory level

      • Intermediate level

      • Advanced level

    • 3.9 REVIEW QUESTIONS

    • 3.10 EXERCISES

  • 4 Earth’s age, thermal and electrical properties

    • 4.1 GEOCHRONOLOGY

      • 4.1.1 Time

        • 4.1.1.1 The clock

        • 4.1.1.2 Units of time

        • 4.1.1.3 The geological timescale

      • 4.1.2 Estimating the Earth’s age

        • 4.1.2.1 Cooling of the Sun

        • 4.1.2.2 Cooling of the Earth

        • 4.1.2.3 Increase of the Earth–Moon separation

        • 4.1.2.4 Oceanic salinity

        • 4.1.2.5 Sedimentary accumulation

      • 4.1.3 Radioactivity

        • 4.1.3.1 Radioactive decay

      • 4.1.4 Radiometric age determination

        • 4.1.4.1 Radioactive carbon

        • 4.1.4.2 The mass spectrometer

        • 4.1.4.3 Rubidium–strontium

        • 4.1.4.4 Potassium–argon

        • 4.1.4.5 Argon–argon

        • 4.1.4.6 Uranium–lead: the concordia–discordia diagram

      • 4.1.5 Ages of the Earth and solar system

    • 4.2 THE EARTH’S HEAT

      • 4.2.1 introduction

      • 4.2.2 Thermodynamic principles

      • 4.2.3 Temperature inside the Earth

        • 4.2.3.1 The adiabatic temperature gradient

        • 4.2.3.2 The melting point gradient

      • 4.2.4 Heat transport in the Earth

        • 4.2.4.1 Conduction

        • 4.2.4.2 Convection

        • 4.2.4.3 Radiation

      • 4.2.5 Sources of heat in the Earth

        • 4.2.5.1 Radioactive heat production

      • 4.2.6 The heat conduction equation

        • 4.2.6.1 Penetration of external heat into the Earth

        • 4.2.6.2 Cooling of the oceanic lithosphere

      • 4.2.7 Continental heat flow

        • 4.2.7.1 Reconstruction of ground surface temperature changes from borehole temperature profiles

        • 4.2.7.2 Variation of continental heat flow with age

        • 4.2.7.3 Heat transfer through porous crustal rocks

      • 4.2.8 Oceanic heat flow

        • 4.2.8.1 Variation of oceanic heat flow and depth with lithospheric age

        • 4.2.8.2 Global heat flow

        • 4.2.8.3 Models for the cooling of oceanic lithosphere

        • 4.2.8.4 Thermal structure of oceanic lithosphere

        • 4.2.8.5 Heat flow at subduction zones

      • 4.2.9 Mantle convection

        • 4.2.9.1 Thermal convection

        • 4.2.9.2 Convection at high Rayleigh numbers

        • 4.2.9.3 Models of mantle convection

        • 4.2.9.4 Mantle plumes

    • 4.3 GEOELECTRICITY

      • 4.3.1 Introduction

      • 4.3.2 Electrical principles

        • 4.3.2.1 Electric field and potential

        • 4.3.2.2 Ohm’s law

        • 4.3.2.3 Types of electrical conduction

      • 4.3.3 Electrical properties of the Earth

        • 4.3.3.1 Electrical surveying

      • 4.3.4 Natural potentials and currents

        • 4.3.4.1 Self-potential (spontaneous potential)

        • 4.3.4.2 SP surveying

        • 4.3.4.3 Telluric currents

      • 4.3.5 Resistivity surveying

        • 4.3.5.1 Potential of a single electrode

        • 4.3.5.2 The general four-electrode method

        • 4.3.5.3 Special electrode configurations

        • 4.3.5.4 Current distribution

        • 4.3.5.5 Apparent resistivity

        • 4.3.5.6 Vertical electrical sounding

        • 4.3.5.7 Induced polarization

        • 4.3.5.8 Electrical resistivity tomography

      • 4.3.6 Electromagnetic surveying

        • 4.3.6.1 Electromagnetic induction

        • 4.3.6.2 EM induction surveying

        • 4.3.6.3 Magnetotelluric sounding

        • 4.3.6.4 Ground-penetrating radar

      • 4.3.7 Electrical conductivity in the Earth

    • 4.4 SUGGESTIONS FOR FURTHER READING

      • Introductory level

      • Intermediate level

      • Advanced level

    • 4.5 REVIEW QUESTIONS

    • 4.6 EXERCISES

      • Geochronology

      • The Earth’s heat

      • Geoelectricity

  • 5 Geomagnetism and paleomagnetism

    • 5.1 HISTORICAL INTRODUCTION

      • 5.1.1 The discovery of magnetism

      • 5.1.2 Pioneering studies in terrestrial magnetism

      • 5.1.3 The physical origins of magnetism

    • 5.2 THE PHYSICS OF MAGNETISM

      • 5.2.1 Introduction

      • 5.2.2 Coulomb’s law for magnetic poles

        • 5.2.2.1 The field of a magnetic pole

        • 5.2.2.2 The potential of a magnetic pole

      • 5.2.3 The magnetic dipole

      • 5.2.4 The magnetic field of an electrical current

      • 5.2.5 Magnetization and the magnetic field inside a material

      • 5.2.6 The magnetic properties of materials

        • 5.2.6.1 Diamagnetism

        • 5.2.6.2 Paramagnetism

        • 5.2.6.3 Ferromagnetism

        • 5.2.6.4 Antiferromagnetism

        • 5.2.6.5 Parasitic ferromagnetism

        • 5.2.6.6 Ferrimagnetism

      • 5.2.7 Magnetic anisotropy

        • 5.2.7.1 Magnetocrystalline anisotropy

        • 5.2.7.2 Magnetostatic (shape) anisotropy

        • 5.2.7.3 Magnetostrictive anisotropy

    • 5.3 ROCK MAGNETISM

      • 5.3.1 The magnetic properties of rocks

      • 5.3.2 The ternary oxide system of magnetic minerals

        • 5.3.2.1 The titanomagnetite series

        • 5.3.2.2 The titanohematite series

      • 5.3.3 Other ferrimagnetic minerals

      • 5.3.4 Identification of ferrimagnetic minerals

      • 5.3.5 Grain size dependence of ferrimagnetic properties

        • 5.3.5.1 Superparamagnetism

        • 5.3.5.2 Single domain particles

        • 5.3.5.3 Multidomain particles

      • 5.3.6 Remanent magnetizations in rocks

        • 5.3.6.1 Thermoremanent magnetization

        • 5.3.6.2 Sedimentary remanent magnetizations

        • 5.3.6.3 Chemical remanent magnetization

        • 5.3.6.4 Isothermal remanent magnetization

        • 5.3.6.5 Other remanent magnetizations

      • 5.3.7 Environmental magnetism

    • 5.4 GEOMAGNETISM

      • 5.4.1 Introduction

      • 5.4.2 Separation of the magnetic fields of external and internal origin

      • 5.4.3 The magnetic field of external origin

        • 5.4.3.1 The Van Allen radiation belts

        • 5.4.3.2 The ionosphere

        • 5.4.3.3 Diurnal variation and magnetic storms

      • 5.4.4 The magnetic field of internal origin

        • 5.4.4.1 The dipole field

        • 5.4.4.2 The non-dipole field

      • 5.4.5 Secular variation

        • 5.4.5.1 Secular variation of the dipole field

        • 5.4.5.2 Secular variation of the non-dipole field

      • 5.4.6 Origin of the internal field

        • 5.4.6.1 Magnetostatic and electromagnetic models

        • 5.4.6.2 The geomagnetic dynamo

        • 5.4.6.3 Computer simulation of the geodynamo

      • 5.4.7 Magnetic fields of the Sun, Moon and planets

        • 5.4.7.1 Magnetic field of the Sun

        • 5.4.7.2 Lunar magnetism

        • 5.4.7.3 Extra-terrestrial magnetic exploration

        • 5.4.7.4 The magnetic fields of the planets

    • 5.5 MAGNETIC SURVEYING

      • 5.5.1 The magnetization of the Earth’s crust

      • 5.5.2 Magnetometers

        • 5.5.2.1 The flux-gate magnetometer

        • 5.5.2.2 The proton-precession magnetometer

        • 5.5.2.3 The absorption-cell magnetometer

      • 5.5.3 Magnetic surveying

        • 5.5.3.1 Measurement methods

        • 5.5.3.2 Magnetic gradiometers

        • 5.5.3.3 The survey pattern

      • 5.5.4 Reduction of magnetic field measurements

      • 5.5.5 Magnetic anomalies

        • 5.5.5.1 Magnetic anomaly of a surface distribution of magnetic poles

        • 5.5.5.2 Magnetic anomaly of a vertical dike

        • 5.5.5.3 Magnetic anomaly of an inclined magnetization

        • 5.5.5.4 Magnetic anomalies of simple geometric bodies

        • 5.5.5.5 Effect of block width on anomaly shape

      • 5.5.6 Oceanic magnetic anomalies

    • 5.6 PALEOMAGNETISM

      • 5.6.1 Introduction

      • 5.6.2 The time-averaged geomagnetic field

        • 5.6.2.1 Archeomagnetic records of secular variation

        • 5.6.2.2 The axial geocentric dipole hypothesis

      • 5.6.3 Methods of paleomagnetism

        • 5.6.3.1 Measurement of remanent magnetization

        • 5.6.3.2 Stepwise progressive demagnetization

        • 5.6.3.3 Analysis of magnetization components

        • 5.6.3.4 Statistical analysis of paleomagnetic directions

        • 5.6.3.5 Field tests of magnetization stability

      • 5.6.4 Paleomagnetism and tectonics

        • 5.6.4.1 Location of the virtual geomagnetic pole

        • 5.6.4.2 Apparent polar wander paths

        • 5.6.4.3 Paleogeographic reconstructions using APW paths

        • 5.6.4.4 Paleomagnetism and continental drift

    • 5.7 GEOMAGNETIC POLARITY

      • 5.7.1 Introduction

        • 5.7.1.1 Geomagnetic polarity transitions

        • 5.7.1.2 Geomagnetic polarity intervals

      • 5.7.2 Magnetostratigraphy in lavas and sediments

      • 5.7.3 Marine magnetic anomalies and geomagnetic polarity history

        • 5.7.3.1 Marine magnetic anomalies

        • 5.7.3.2 Uniformity of sea-floor spreading

        • 5.7.3.3 The marine record of geomagnetic polarity history

      • 5.7.4 Geomagnetic polarity timescales

        • 5.7.4.1 Magnetostratigraphic calibration of polarity sequences

        • 5.7.4.2 Reconstruction of plate tectonic motions

      • 5.7.5 Frequency of polarity reversals

      • 5.7.6 Early Mesozoic and Paleozoic reversal history

    • 5.8 SUGGESTIONS FOR FURTHER READING

      • Introductory level

      • Intermediate level

      • Advanced level

    • 5.9 REVIEW QUESTIONS

    • 5.10 EXERCISES

  • Appendix A The three-dimensional wave equations

    • Derivation of general equations of motion

    • Equation of longitudinal waves

    • Equation of transverse waves

  • Appendix B Cooling of a semi-infinite half-space

    • Evaluation of the integral Y0 in Eq. (B17)

  • Bibliography

  • Index

Nội dung

This page intentionally left blank Fundamentals of Geophysics Second Edition This second edition of Fundamentals of Geophysics has been completely revised and updated, and is the ideal geophysics textbook for undergraduate students of geoscience with only an introductory level of knowledge in physics and mathematics Presenting a comprehensive overview of the fundamental principles of each major branch of geophysics (gravity, seismology, geochronology, thermodynamics, geoelectricity, and geomagnetism), this text also considers geophysics within the wider context of plate tectonics, geodynamics, and planetary science Basic principles are explained with the aid of numerous figures, and important geophysical results are illustrated with examples from scientific literature Step-by-step mathematical treatments are given where necessary, allowing students to easily follow the derivations Text boxes highlight topics of interest for more advanced students Each chapter contains a short historical summary and ends with a reading list that directs students to a range of simpler, alternative, or more advanced, resources This new edition also includes review questions to help evaluate the reader’s understanding of the topics covered, and quantitative exercises at the end of each chapter Solutions to the exercises are available to instructors   is Professor Emeritus of Geophysics at the Institute of Geophysics at the Swiss Federal Institute of Technology (ETH), Zürich, where he has taught and carried out research for over 30 years His research interests include rock magnetism, magnetostratigraphy, and tectonic applications of paleomagnetic methods Fundamentals of Geophysics Second Edition WI L LI A M LOWR I E Swiss Federal Institute of Technology, Zürich CAMBRIDGE UNIVERSITY PRESS Cambridge, New York, Melbourne, Madrid, Cape Town, Singapore, São Paulo Cambridge University Press The Edinburgh Building, Cambridge CB2 8RU, UK Published in the United States of America by Cambridge University Press, New York www.cambridge.org Information on this title: www.cambridge.org/9780521859028 © W Lowrie 2007 This publication is in copyright Subject to statutory exception and to the provision of relevant collective licensing agreements, no reproduction of any part may take place without the written permission of Cambridge University Press First published in print format 2007 eBook (EBL) ISBN-13 978-0-511-35447-2 ISBN-10 0-511-35447-9 eBook (EBL) ISBN-13 ISBN-10 hardback 978-0-521-85902-8 hardback 0-521-85902-6 ISBN-13 ISBN-10 paperback 978-0-521-67596-3 paperback 0-521-67596-0 Cambridge University Press has no responsibility for the persistence or accuracy of urls for external or third-party internet websites referred to in this publication, and does not guarantee that any content on such websites is, or will remain, accurate or appropriate Contents Preface Acknowledgements page vii ix The Earth as a planet 1.1 1.2 1.3 1.4 1.5 The solar system The dynamic Earth Suggestions for further reading Review questions Exercises 1 15 40 41 41 Gravity, the figure of the Earth and geodynamics 43 2.1 2.2 2.3 2.4 2.5 2.6 2.7 2.8 2.9 2.10 2.11 The Earth’s size and shape Gravitation The Earth’s rotation The Earth’s figure and gravity Gravity anomalies Interpretation of gravity anomalies Isostasy Rheology Suggestions for further reading Review questions Exercises 43 45 48 61 73 84 99 105 117 118 118 Seismology and the internal structure of the Earth 121 3.1 3.2 3.3 3.4 3.5 3.6 3.7 3.8 3.9 3.10 Introduction Elasticity theory Seismic waves The seismograph Earthquake seismology Seismic wave propagation Internal structure of the Earth Suggestions for further reading Review questions Exercises 121 122 130 140 148 171 186 201 202 203 Earth’s age, thermal and electrical properties 207 4.1 4.2 4.3 4.4 4.5 4.6 Geochronology The Earth’s heat Geoelectricity Suggestions for further reading Review questions Exercises 207 220 252 276 276 277 v vi Contents Geomagnetism and paleomagnetism 281 5.1 5.2 5.3 5.4 5.5 5.6 5.7 5.8 5.9 5.10 Historical introduction The physics of magnetism Rock magnetism Geomagnetism Magnetic surveying Paleomagnetism Geomagnetic polarity Suggestions for further reading Review questions Exercises 281 283 293 305 320 334 349 359 359 360 Appendix A The three-dimensional wave equations Appendix B Cooling of a semi-infinite half-space 363 366 Bibliography 368 Index 375 Preface to the second edition In the ten years that have passed since the publication of the first edition of this textbook exciting advances have taken place in every discipline of geophysics Computer-based improvements in technology have led the way, allowing more sophistication in the acquisition and processing of geophysical data Advances in mass spectrometry have made it possible to analyze minute samples of matter in exquisite detail and have contributed to an improved understanding of the origin of our planet and the evolution of the solar system Space research has led to better knowledge of the other planets in the solar system, and has revealed distant objects in orbit around the Sun As a result, the definition of a planet has been changed Satellite-based technology has provided more refined measurement of the gravity and magnetic fields of the Earth, and has enabled direct observation from space of minute surface changes related to volcanic and tectonic events The structure, composition and dynamic behavior of the deep interior of the Earth have become better understood owing to refinements in seismic tomography Fast computers and sophisticated algorithms have allowed scientists to construct plausible models of slow geodynamic behavior in the Earth’s mantle and core, and to elucidate the processes giving rise to the Earth’s magnetic field The application of advanced computer analysis in high-resolution seismic reflection and ground-penetrating radar investigations has made it possible to describe subtle features of environmental interest in near-surface structures Rock magnetic techniques applied to sediments have helped us to understand slow natural processes as well as more rapid anthropological changes that affect our environment, and to evaluate climates in the distant geological past Climatic history in the more recent past can now be deduced from the analysis of temperature in boreholes Although the many advances in geophysical research depend strongly on the aid of computer science, the fundamental principles of geophysical methods remain the same; they constitute the foundation on which progress is based In revising this textbook, I have heeded the advice of teachers who have used it and who recommended that I change as little as possible and only as much as necessary (to paraphrase medical advice on the use of medication) The reviews of the first edition, the feedback from numerous students and teachers, and the advice of friends and colleagues helped me greatly in deciding what to The structure of the book has been changed slightly compared to the first edition The final chapter on geodynamics has been removed and its contents integrated into the earlier chapters, where they fit better Text-boxes have been introduced to handle material that merited further explanation, or more extensive treatment than seemed appropriate for the body of the text Two appendices have been added to handle more adequately the three-dimensional wave equation and the cooling of a half-space, respectively At the end of each chapter is a list of review questions that should help students to evaluate their knowledge of what they have read Each chapter is also accompanied by a set of exercises They are intended to provide practice in handling some of the numerical aspects of the topics discussed vii viii Preface in the chapter They should help the student to become more familiar with geophysical techniques and to develop a better understanding of the fundamental principles The first edition was mostly free of errata, in large measure because of the patient, accurate and meticulous proofreading by my wife Marcia, whom I sincerely thank Some mistakes still occurred, mostly in the more than 350 equations, and were spotted and communicated to me by colleagues and students in time to be corrected in the second printing of the first edition Regarding the students, this did not improve (or harm) their grades, but I was impressed and pleased that they were reading the book so carefully Among the colleagues, I especially thank Bob Carmichael for painstakingly listing many corrections and Ray Brown for posing important questions Constructive criticisms and useful suggestions for additions and changes to the individual revised chapters in this edition were made by Mark Bukowinski, Clark Wilson, Doug Christensen, Jim Dewey, Henry Pollack, Ladislaus Rybach, Chris Heinrich, Hans-Ruedi Maurer and Mike Fuller I am very grateful to these colleagues for the time they expended and their unselfish efforts to help me If errors persist in this edition, it is not their fault but due to my negligence The publisher of this textbook, Cambridge University Press, is a not-for-profit charitable institution One of their activities is to promote academic literature in the “third world.” With my agreement, they decided to publish a separate low-cost version of the first edition, for sale only in developing countries This version accounted for about one-third of the sales of the first edition As a result, earth science students in developing countries could be helped in their studies of geophysics; several sent me appreciative messages, which I treasure The bulk of this edition has been written following my retirement two years ago, after 30 years as professor of geophysics at ETH Zürich My new emeritus status should have provided lots of time for the project, but somehow it took longer than I expected My wife Marcia exhibited her usual forbearance and understanding for my obsession I thank her for her support, encouragement and practical suggestions, which have been as important for this as for the first edition This edition is dedicated to her, as well as to my late parents William Lowrie Zürich August, 2006 ... tectonic applications of paleomagnetic methods Fundamentals of Geophysics Second Edition WI L LI A M LOWR I E Swiss Federal Institute of Technology, Zürich CAMBRIDGE UNIVERSITY PRESS Cambridge, New... Singapore, São Paulo Cambridge University Press The Edinburgh Building, Cambridge CB2 8RU, UK Published in the United States of America by Cambridge University Press, New York www .cambridge. org Information... intentionally left blank Fundamentals of Geophysics Second Edition This second edition of Fundamentals of Geophysics has been completely revised and updated, and is the ideal geophysics textbook for

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