The Seismogenic Zone of Subduction Thrust Faults

Kobo ebook | August 7, 2012

byTimothy H Dixon, Casey Moore

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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.

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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 earthqu...

Timothy H. Dixon is a professor of tectonics, geodesy, and remote sensing at the Rosenstiel School of Marine and Atmospheric Science, which is associated with the University of Miami.J. Casey Moore is professor of earth sciences at the University of California Santa Cruz.
Format:Kobo ebookPublished:August 7, 2012Publisher:Columbia University PressLanguage:English

The following ISBNs are associated with this title:

ISBN - 10:0231512015

ISBN - 13:9780231512015

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Table of Contents

The Thermal State of 1824 Ma Upper Lithosphere
Influence of Subducting Topography on Earthquake
Pore Pressure and Fluid Flow in the Northern Barbados
Pore Pressure within Underthrust Sediment in Subduction
Deformation and Mechanical Strength of Sediments at
Seismic Reflection Imaging
How Accretionary Prisms Elucidate Seismogenesis
A Review
Seismic and Geodetic Studies
Anomalous Earthquake Ruptures at Shallow Depths
Secular Transient and Seasonal Crustal Movements in Japan
Elastic and Viscoelastic Models of Crustal Deformation
Distinct Updip Limits to Geodetic Locking and Microseismicity
Regional Scale Deformation
Subduction and Mountain Building in the Central Andes
List of Contributors