The Seismogenic Zone of Subduction Thrust Faults / / ed. by J. Casey Moore, Timothy Dixon.

• Superior document: Title is part of eBook package: De Gruyter Columbia University Press eBook-Package Backlist 2000-2013
• MitwirkendeR: Ahmed, Imtiaz,; Ask, Maria V. S.,; Beeler, N. M.,; Bekins, Barbara A.,; Berhorst, Arnim,; Bilek, Susan L.,; Bilek, Susan,; DeShon, H.,; DeShon, Heather R.,; Diamente, C.,; Dixon, Timothy H.,; Fisher, A. T.,; Flueh, Ernst R.,; Harris, R.,; Hasegawa, Akira,; Heki, Kosuke,; Hyndman, R. D.,; Igarashi, Toshihiro,; Kelly, Robyn K.,; Kley, Jonas,; Lay, Thorne,; Lockner, David A.,; MacKnight, R.,; Marone, Chris,; Matsuzawa, Toru,; McIntosh, Kirk D.,; Meneghini, Francesca,; Miura, Satoshi,; Moore, Diane E.,; Moore, J. Casey,; Morgan, Julia K.,; Okada, Tomomi,; Pfender, M.,; Pisani, P. Costa,; Ramsey, E. Blanche,; Ranero, Cesar R.,; Rowe, Christie,; Saffer, Demian M.,; Schwartz, Susan Y.,; Screaton, Elizabeth J.,; Seno, Tetsuzo,; Silver, E.,; Silver, Eli A.,; Spinelli, G.,; Stein, C. A.,; Suwa, Yoko,; Uchida, Naoki,; Underwood, Michael B.,; Vietor, Tim,; Villinger, H.,; Wang, K.,; Wang, Kelin,
• HerausgeberIn: Dixon, Timothy,; Moore, J. Casey,
• Place / Publishing House: New York, NY : : Columbia University Press, , [2007]; ©2007
• Year of Publication: 2007
• Language: English
• Series: MARGINS Theoretical and Experimental Earth Science Series
• Physical Description: 1 online resource (692 p.) :; 10 tables, 242 figures, and 3 plates
• Other title: Frontmatter --; Contents --; Preface --; Part I. Introduction --; 1. The Seismogenic Zone of Subduction Thrust Faults --; 2. The Seismogenic Zone of Subduction Thrust Faults --; Part II. The Incoming Plate --; 3. Sediment Inputs to Subduction Zones --; 4. The Thermal State of 18-24 Ma Upper Lithosphere Subducting Below the Nicoya Peninsula, Northern Costa Rica Margin --; 5. Influence of Subducting Topography on Earthquake Rupture --; Part III. Convergent Margin Structure, Fluids, and Subduction Thrust Evolution --; 6. Pore Pressure and Fluid Flow in the Northern Barbados Accretionary Complex --; 7. Pore Pressure within Underthrust Sediment in Subduction Zones --; 8. Deformation and Mechanical Strength of Sediments at the Nankai Subduction Zone --; 9. The Nicaragua Convergent Margin --; 10. How Accretionary Prisms Elucidate Seismogenesis in Subduction Zones --; Part IV. Laboratory Studies --; 11. Friction of the Smectite Clay Montmorillonite --; 12. Fault Friction and the Upper Transition from Seismic to Aseismic Faulting --; 13. Laboratory-Observed Faulting in Intrinsically and Apparently Weak Materials --; Part V. Seismic and Geodetic Studies --; 14. Asperities and Quasi-Static Slips on the Subducting Plate Boundary East of Tohoku, Northeast Japan --; 15. Anomalous Earthquake Ruptures at Shallow Depths on Subduction Zone Megathrusts --; 16. Secular, Transient, and Seasonal Crustal Movements in Japan from a Dense GPS Array --; 17. Elastic and Viscoelastic Models of Crustal Deformation in Subduction Earthquake Cycles --; 18. Distinct Updip Limits to Geodetic Locking and Microseismicity at the Northern Costa Rica Seismogenic Zone --; Part VI. Regional Scale Deformation --; 19. Collision Versus Subduction --; Subduction and Mountain Building in the Central Andes --; Contributors --; Index
• Format: Mode of access: Internet via World Wide Web.
• ISBN: 9780231512015; 9783110442472
• DOI: 10.7312/dixo13866
• Access: restricted access
• Hierarchical level: Monograph
• Statement of Responsibility: ed. by J. Casey Moore, Timothy Dixon.

Subduction zones, one of the three types of plate boundaries, return Earth's surface to its deep interior. Because subduction zones are gently inclined at shallow depths and depress Earth's temperature gradient, they have the largest seismogenic area of any plate boundary. Consequently, subduction zones generate Earth's largest earthquakes and most destructive tsunamis. As tragically demonstrated by the Sumatra earthquake and tsunami of December 2004, these events often impact densely populated coastal areas and cause large numbers of fatalities. While scientists have a general understanding of the seismogenic zone, many critical details remain obscure. This volume attempts to answer such fundamental concerns as why some interplate subduction earthquakes are relatively modest in rupture length (greater than 100 km) while others, such as the great (M greater than 9) 1960 Chile, 1964 Alaska, and 2004 Sumatra events, rupture along 1000 km or more. Contributors also address why certain subduction zones are fully locked, accumulating elastic strain at essentially the full plate convergence rate, while others appear to be only partially coupled or even freely slipping; whether these locking patterns persist through the seismic cycle; and what is the role of sediments and fluids on the incoming plate.Nineteen papers written by experts in a variety of fields review the most current lab, field, and theoretical research on the origins and mechanics of subduction zone earthquakes and suggest further areas of exploration. They consider the composition of incoming plates, laboratory studies concerning sediment evolution during subduction and fault frictional properties, seismic and geodetic studies, and regional scale deformation. The forces behind subduction zone earthquakes are of increasing environmental and societal importance.