Cover image for Earthquake and volcano deformation
Title:
Earthquake and volcano deformation
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Publication Information:
Princeton, N.J. : Princeton University Press, c2010
Physical Description:
xxiii, 432 p. : ill., maps ; 26 cm.
ISBN:
9780691133027

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30000010274293 QE604 S44 2010 Open Access Book Book
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Summary

Summary

Earthquake and Volcano Deformation is the first textbook to present the mechanical models of earthquake and volcanic processes, emphasizing earth-surface deformations that can be compared with observations from Global Positioning System (GPS) receivers, Interferometric Radar (InSAR), and borehole strain- and tiltmeters. Paul Segall provides the physical and mathematical fundamentals for the models used to interpret deformation measurements near active faults and volcanic centers.

Segall highlights analytical methods of continuum mechanics applied to problems of active crustal deformation. Topics include elastic dislocation theory in homogeneous and layered half-spaces, crack models of faults and planar intrusions, elastic fields due to pressurized spherical and ellipsoidal magma chambers, time-dependent deformation resulting from faulting in an elastic layer overlying a viscoelastic half-space and related earthquake cycle models, poroelastic effects due to faulting and magma chamber inflation in a fluid-saturated crust, and the effects of gravity on deformation. He also explains changes in the gravitational field due to faulting and magmatic intrusion, effects of irregular surface topography and earth curvature, and modern concepts in rate- and state-dependent fault friction. This textbook presents sample calculations and compares model predictions against field data from seismic and volcanic settings from around the world.

Earthquake and Volcano Deformation requires working knowledge of stress and strain, and advanced calculus. It is appropriate for advanced undergraduates and graduate students in geophysics, geology, and engineering.

Professors: A supplementary Instructor's Manual is available for this book. It is restricted to teachers using the text in courses. For information on how to obtain a copy, refer to: https://press.princeton.edu/class_use/solutions.html


Author Notes

Paul Segall is professor of geophysics at Stanford University.


Reviews 1

Choice Review

An understanding and modeling of Earth's crustal deformation connected with earthquakes and volcanic activity has enabled significantly improved precision in the application of space-based geodetic systems. Segall (geophysics, Stanford Univ.) provides this first work on the topic that highlights, from a thorough mathematical basis, new insights into the basic theory of mechanical models and applications of GPS and InSAR to improve understanding of Earth's deformation processes. The 12-chapter work begins with "Deformation, Stress, and Conservation Laws." The next two chapters cover strike-slip and dip-slip fault dislocation models. The remaining chapters are titled "Crack Models of Faults," "Elastic Heterogeneity," "Postseismic Relaxation," "Volcano Deformation," "Topography and Earth Curvature," "Gravitational Effects," "Poroelastic Effects," "Fault Friction," and "Interseismic Deformation and Plate Boundary Cycle Models." Each chapter is reinforced with an extensive bibliography. This excellent advanced textbook will most positively impact graduate education and basic and applied research into the science of crustal deformation. Summing Up: Highly recommended. Graduate students through professionals/practitioners in geophysics, geology, and rock mechanics engineering. T. L. T. Grose emeritus, Colorado School of Mines


Table of Contents

Prefacep. xi
Acknowledgmentsp. xv
Originsp. xvii
1 Deformation, Stress, and Conservation Lawsp. 1
1.1 Strainp. 2
1.1.1 Strains in Curvilinear Coordinatesp. 7
1.2 Rotationp. 9
1.3 Stressp. 13
1.4 Coordinate Transformationsp. 16
1.5 Principal Strains and Stressesp. 18
1.6 Compatibility Equationsp. 21
1.7 Conservation Lawsp. 21
1.7.1 Equilibrium Equations in Curvilinear Coordinatesp. 24
1.8 Constitutive Lawsp. 24
1.9 Reciprocal Theoremp. 27
1.10 Problemsp. 28
1.11 Referencesp. 30
2 Dislocation Models of Strike-Slip Faultsp. 32
2.1 Full-Space Solutionp. 32
2.2 Half-Space Solutionp. 37
2.2.1 Coseismic Faultingp. 38
2.2.2 Interseismic Deformationp. 39
2.2.3 Postseismic Slipp. 42
2.3 Distributed Slipp. 43
2.4 Application to the San Andreas and Other Strike-Slip Faultsp. 44
2.5 Displacement at Depthp. 47
2.6 Summary and Perspectivep. 49
2.7 Problemsp. 50
2.8 Referencesp. 50
3 Dip-Slip Faults and Dislocations in Three Dimensionsp. 51
3.1 Volterra's Formulap. 52
3.1.1 Body Force Equivalents and Moment Tensorsp. 54
3.2 Screw Dislocationsp. 59
3.3 Two-Dimensional Edge Dislocationsp. 60
3.3.1 Dipping Faultp. 63
3.4 Coseismic Deformation Associated with Dipping Faultsp. 67
3.5 Displacements and Stresses Due to Edge Dislocation at Depthp. 71
3.6 Dislocations in Three Dimensionsp. 75
3.6.1 Full-Space Green's Functionsp. 75
3.6.2 Half-Space Green's Functionsp. 77
3.6.3 Point-Source Dislocationsp. 78
3.6.4 Finite Rectangular Dislocationsp. 80
3.6.5 Examplesp. 82
3.6.6 Distributed Slipp. 84
3.7 Strain Energy Change Due to Faultingp. 86
3.8 Summary and Perspectivep. 87
3.9 Problemsp. 87
3.10 Referencesp. 90
4 Crack Models of Faultsp. 92
4.1 Boundary Integral Methodp. 92
4.1.1 Inversion of the Integral Equationp. 97
4.2 Displacement on the Earth's Surfacep. 98
4.3 A Brief Introduction to Fracture Mechanicsp. 99
4.4 Nonsingular Stress Distributionsp. 105
4.5 Comparison of Slip Distributions and Surface Displacementsp. 107
4.6 Boundary Element Methodsp. 110
4.7 Fourier Transform Methodsp. 111
4.8 Some Three-Dimensional Crack Resultsp. 113
4.9 Summary and Perspectivep. 114
4.10 Problemsp. 115
4.11 Referencesp. 117
5 Elastic Heterogeneityp. 118
5.1 Long Strike-Slip Fault Bounding Two Mediap. 118
5.2 Strike-Slip Fault within a Compliant Fault Zonep. 120
5.3 Strike-Slip Fault beneath a Layerp. 125
5.4 Strike-Slip within a Layer over Half-Spacep. 129
5.5 Propagator Matrix Methodsp. 131
5.5.1 The Propagator Matrix for Antiplane Deformationp. 135
5.5.2 Vertical Fault in a Homogeneous Half-Spacep. 136
5.5.3 Vertical Fault within Half-Space beneath a Layerp. 138
5.5.4 Vertical Fault in Layer over Half-Spacep. 139
5.5.5 General Solution for an Arbitrary Number of Layersp. 141
5.5.6 Displacements and Stresses at Depthp. 143
5.5.7 Propagator Methods for Plane Strainp. 143
5.6 Propagator Solutions in Three Dimensionsp. 150
5.7 Approximate Solutions for Arbitrary Variations in Propertiesp. 154
5.7.1 Variations in Shear Modulusp. 157
5.7.2 Screw Dislocationp. 158
5.7.3 Edge Dislocationp. 159
5.8 Summary and Perspectivep. 159
5.9 Problemsp. 162
5.10 Referencesp. 164
6 Postseismic Relaxationp. 166
6.1 Elastic Layer over Viscous Channelp. 169
6.2 Viscoelasticityp. 172
6.2.1 Correspondence Principlep. 175
6.3 Strike-Slip Fault in an Elastic Plate Overlying a Viscoelastic Half-Spacep. 176
6.3.1 Stress in Plate and Half-Spacep. 181
6.4 Strike-Slip Fault in Elastic Layer Overlying a Viscoelastic Channelp. 182
6.5 Dip-Slip Faultingp. 187
6.5.1 Examplesp. 190
6.6 Three-Dimensional Calculationsp. 191
6.7 Summary and Perspectivep. 193
6.8 Problemsp. 197
6.9 Referencesp. 198
7 Volcano Deformationp. 200
7.1 Spherical Magma Chamberp. 203
7.1.1 Center of Dilatationp. 208
7.1.2 Volume of the Uplift, Magma Chamber, and Magmap. 212
7.2 Ellipsoidal Magma Chambersp. 214
7.3 Magmatic Pipes and Conduitsp. 225
7.4 Dikes and Sillsp. 229
7.4.1 Crack Models of Dikes and Sillsp. 231
7.4.2 Surface Fracturing and Dike Intrusionp. 236
7.5 Other Magma Chamber Geometriesp. 237
7.6 Viscoelastic Relaxation around Magma Chambersp. 240
7.7 Summary and Perspectivep. 248
7.8 Problemsp. 249
7.9 Referencesp. 252
8 Topography and Earth Curvaturep. 255
8.1 Scaling Considerationsp. 259
8.2 Implementation Considerationsp. 260
8.3 Center of Dilatation beneath a Volcanop. 260
8.4 Earth's Sphericityp. 261
8.5 Summary and Perspectivep. 263
8.6 Problemsp. 265
8.7 Referencesp. 265
9 Gravitational Effectsp. 267
9.1 Nondimensional Form of Equilibrium Equationsp. 270
9.2 Inclusion in Propagator Matrix Formulationp. 273
9.3 Surface Gravity Approximationp. 275
9.4 Gravitational Effects in Viscoelastic Solutionsp. 276
9.4.1 Incompressible Half-Spacep. 277
9.4.2 No-Buoyancy Approximationp. 278
9.4.3 Wang Approachp. 279
9.4.4 Comparison of Different Viscoelastic Modelsp. 280
9.4.5 Relaxed Viscoelastic Responsep. 282
9.5 Changes in Gravity Induced by Deformationp. 283
9.5.1 Gravity Changes and Volcano Deformationp. 289
9.5.2 An Example from Long Valley Caldera, Californiap. 292
9.6 Summary and Perspectivep. 292
9.7 Problemsp. 294
9.8 Referencesp. 295
10 Poroelastic Effectsp. 297
10.1 Constitutive Lawsp. 300
10.1.1 Macroscopic Descriptionp. 300
10.1.2 Micromechanical Descriptionp. 303
10.2 Field Equationsp. 305
10.3 Analogy to Thermoelasticityp. 308
10.4 One-Dimensional Deformationp. 309
10.4.1 Step Load on the Free Surfacep. 310
10.4.2 Time-Varying Fluid Load on the Free Surfacep. 312
10.5 Dislocations in Two Dimensionsp. 313
10.6 Inflating Magma Chamber in a Poroelastic Half-Planep. 315
10.7 Cumulative Poroelastic Deformation in Three Dimensionsp. 321
10.8 Specified Pore Pressure Changep. 324
10.9 Summary and Perspectivep. 328
10.10 Problemsp. 329
10.11 Referencesp. 330
11 Fault Frictionp. 332
11.1 Slip-Weakening Frictionp. 333
11.2 Velocity-Weakening Frictionp. 335
11.3 Rate and State Frictionp. 336
11.3.1 Linearized Stability Analysisp. 344
11.4 Implications for Earthquake Nucleationp. 347
11.5 Nonlinear Stability Analysisp. 357
11.6 Afterslipp. 360
11.7 Transient Slip Eventsp. 366
11.8 Summary and Perspectivep. 367
11.9 Problemsp. 368
11.10 Referencesp. 369
12 Interseismic Deformation and Plate Boundary Cycle Modelsp. 372
12.1 Elastic Dislocation Modelsp. 372
12.1.1 Dip-Slip Faultsp. 373
12.2 Plate Motionsp. 376
12.3 Elastic Block Modelsp. 378
12.4 Viscoelastic Cycle Modelsp. 380
12.4.1 Viscoelastic Strike-Slip Earthquake Cycle Modelsp. 380
12.4.2 Comparison to Data from San Andreas Faultp. 386
12.4.3 Viscoelastic Models with Stress-Driven Deep-Fault Creepp. 389
12.4.4 Viscoelastic Cycle Models for Dipping Faultsp. 394
12.5 Rate-State Friction Earthquake Cycle Modelsp. 407
12.6 Summary and Perspectivep. 409
12.7 Problemsp. 412
12.8 Referencesp. 413
Appendix A Integral Transformsp. 415
A.1 Fourier Transformsp. 415
A.2 Laplace Transformsp. 416
A.3 Referencesp. 419
Appendix B A Solution of the Diffusion Equationp. 420
Appendix C Displacements Due to Crack Model of Strike-Slip Fault by Contour Integrationp. 423
Indexp. 425