Chapter
Licensed
Unlicensed
Requires Authentication
13. Laboratory-Observed Faulting in Intrinsically and Apparently Weak Materials
Strength, Seismic Coupling, Dilatancy, and Pore-Fluid Pressure
-
N. M. Beeler
You are currently not able to access this content.
You are currently not able to access this content.
Chapters in this book
- Frontmatter i
- Contents v
- Preface viii
-
Part I. Introduction
- 1. The Seismogenic Zone of Subduction Thrust Faults 2
- 2. The Seismogenic Zone of Subduction Thrust Faults 15
-
Part II. The Incoming Plate
- 3. Sediment Inputs to Subduction Zones 42
- 4. The Thermal State of 18–24 Ma Upper Lithosphere Subducting Below the Nicoya Peninsula, Northern Costa Rica Margin 86
- 5. Influence of Subducting Topography on Earthquake Rupture 123
-
Part III. Convergent Margin Structure, Fluids, and Subduction Thrust Evolution
- 6. Pore Pressure and Fluid Flow in the Northern Barbados Accretionary Complex 148
- 7. Pore Pressure within Underthrust Sediment in Subduction Zones 171
- 8. Deformation and Mechanical Strength of Sediments at the Nankai Subduction Zone 210
- 9. The Nicaragua Convergent Margin 257
- 10. How Accretionary Prisms Elucidate Seismogenesis in Subduction Zones 288
-
Part IV. Laboratory Studies
- 11. Friction of the Smectite Clay Montmorillonite 317
- 12. Fault Friction and the Upper Transition from Seismic to Aseismic Faulting 346
- 13. Laboratory-Observed Faulting in Intrinsically and Apparently Weak Materials 370
-
Part V. Seismic and Geodetic Studies
- 14. Asperities and Quasi-Static Slips on the Subducting Plate Boundary East of Tohoku, Northeast Japan 451
- 15. Anomalous Earthquake Ruptures at Shallow Depths on Subduction Zone Megathrusts 476
- 16. Secular, Transient, and Seasonal Crustal Movements in Japan from a Dense GPS Array 512
- 17. Elastic and Viscoelastic Models of Crustal Deformation in Subduction Earthquake Cycles 540
- 18. Distinct Updip Limits to Geodetic Locking and Microseismicity at the Northern Costa Rica Seismogenic Zone 576
-
Part VI. Regional Scale Deformation
- 19. Collision Versus Subduction 601
- Subduction and Mountain Building in the Central Andes 624
- Contributors 661
- Index 665
Chapters in this book
- Frontmatter i
- Contents v
- Preface viii
-
Part I. Introduction
- 1. The Seismogenic Zone of Subduction Thrust Faults 2
- 2. The Seismogenic Zone of Subduction Thrust Faults 15
-
Part II. The Incoming Plate
- 3. Sediment Inputs to Subduction Zones 42
- 4. The Thermal State of 18–24 Ma Upper Lithosphere Subducting Below the Nicoya Peninsula, Northern Costa Rica Margin 86
- 5. Influence of Subducting Topography on Earthquake Rupture 123
-
Part III. Convergent Margin Structure, Fluids, and Subduction Thrust Evolution
- 6. Pore Pressure and Fluid Flow in the Northern Barbados Accretionary Complex 148
- 7. Pore Pressure within Underthrust Sediment in Subduction Zones 171
- 8. Deformation and Mechanical Strength of Sediments at the Nankai Subduction Zone 210
- 9. The Nicaragua Convergent Margin 257
- 10. How Accretionary Prisms Elucidate Seismogenesis in Subduction Zones 288
-
Part IV. Laboratory Studies
- 11. Friction of the Smectite Clay Montmorillonite 317
- 12. Fault Friction and the Upper Transition from Seismic to Aseismic Faulting 346
- 13. Laboratory-Observed Faulting in Intrinsically and Apparently Weak Materials 370
-
Part V. Seismic and Geodetic Studies
- 14. Asperities and Quasi-Static Slips on the Subducting Plate Boundary East of Tohoku, Northeast Japan 451
- 15. Anomalous Earthquake Ruptures at Shallow Depths on Subduction Zone Megathrusts 476
- 16. Secular, Transient, and Seasonal Crustal Movements in Japan from a Dense GPS Array 512
- 17. Elastic and Viscoelastic Models of Crustal Deformation in Subduction Earthquake Cycles 540
- 18. Distinct Updip Limits to Geodetic Locking and Microseismicity at the Northern Costa Rica Seismogenic Zone 576
-
Part VI. Regional Scale Deformation
- 19. Collision Versus Subduction 601
- Subduction and Mountain Building in the Central Andes 624
- Contributors 661
- Index 665