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7. Thermo-Mechanical Models of Convergent Orogenesis: Thermal and Rheologic Dependence of Crustal Deformation
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Sean D. Willett
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Chapters in this book
- Frontmatter i
- Contents v
- Contributors vii
- Preface ix
- 1. Consequences of Asthenospheric Variability on Continental Rifting 1
- 2. Velocity Fields, Faulting, and Strength on the Continents 31
- 3. Mechanics of Low-Angle Normal Faults 46
- 4. Depth-Dependent Lithospheric Stretching at Rifted Continental Margins 92
- 5. Limits of the Seismogenic Zone 138
- 6. Controls on Subduction Thrust Earthquakes: Downdip Changes in Composition and State 166
- 7. Thermo-Mechanical Models of Convergent Orogenesis: Thermal and Rheologic Dependence of Crustal Deformation 179
- 8. Structure of Large-Displacement, Strike-Slip Fault Zones in the Brittle Continental Crust 223
- 9. The Strength of the San Andreas Fault: A Discussion 261
- 10. Deformation Behavior of Partially Molten Mantle Rocks 284
- 11. Relations Among Porosity, Permeability, and Deformation in Rocks at High Temperatures 311
- Index 341
Chapters in this book
- Frontmatter i
- Contents v
- Contributors vii
- Preface ix
- 1. Consequences of Asthenospheric Variability on Continental Rifting 1
- 2. Velocity Fields, Faulting, and Strength on the Continents 31
- 3. Mechanics of Low-Angle Normal Faults 46
- 4. Depth-Dependent Lithospheric Stretching at Rifted Continental Margins 92
- 5. Limits of the Seismogenic Zone 138
- 6. Controls on Subduction Thrust Earthquakes: Downdip Changes in Composition and State 166
- 7. Thermo-Mechanical Models of Convergent Orogenesis: Thermal and Rheologic Dependence of Crustal Deformation 179
- 8. Structure of Large-Displacement, Strike-Slip Fault Zones in the Brittle Continental Crust 223
- 9. The Strength of the San Andreas Fault: A Discussion 261
- 10. Deformation Behavior of Partially Molten Mantle Rocks 284
- 11. Relations Among Porosity, Permeability, and Deformation in Rocks at High Temperatures 311
- Index 341