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Thermal Evolution of the Tertiary Shimanto Belt, Southwest Japan

Thermal Evolution of the Tertiary Shimanto Belt, Southwest Japan PDF Author: Michael B. Underwood
Publisher: Geological Society of America
ISBN: 9780813722733
Category : Science
Languages : en
Pages : 188

Book Description


Thermal Evolution of the Tertiary Shimanto Belt, Southwest Japan

Thermal Evolution of the Tertiary Shimanto Belt, Southwest Japan PDF Author: Michael B. Underwood
Publisher: Geological Society of America
ISBN: 9780813722733
Category : Science
Languages : en
Pages : 188

Book Description


The Seismogenic Zone of Subduction Thrust Faults

The Seismogenic Zone of Subduction Thrust Faults PDF Author: Timothy H. Dixon
Publisher: Columbia University Press
ISBN: 0231512015
Category : Science
Languages : en
Pages : 691

Book Description
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.

Exhumation Processes

Exhumation Processes PDF Author: Uwe Ring
Publisher: Geological Society of London
ISBN: 9781862390324
Category : Science
Languages : en
Pages : 390

Book Description


Geology of a Transpressional Orogen Developed During Ridge-trench Interaction Along the North Pacific Margin

Geology of a Transpressional Orogen Developed During Ridge-trench Interaction Along the North Pacific Margin PDF Author: Virginia Baker Sisson
Publisher: Geological Society of America
ISBN: 9780813723716
Category : Science
Languages : en
Pages : 392

Book Description
Accompanying CD-ROM contains maps using the comercial drawing program Adobe Illustrator 9.0 for Wintel systems.

Low-Temperature Thermochronology:

Low-Temperature Thermochronology: PDF Author: Peter W. Reiners
Publisher: Walter de Gruyter GmbH & Co KG
ISBN: 1501509578
Category : Science
Languages : en
Pages : 644

Book Description
Volume 58 of Reviews in Mineralogy and Geochemistry presents 22 chapters covering many of the important modern aspects of thermochronology. The coverage of the chapters ranges widely, including historical perspective, analytical techniques, kinetics and calibrations, modeling approaches, and interpretational methods. In general, the chapters focus on intermediate- to low-temperature thermochronometry, though some chapters cover higher temperature methods such as monazite U/Pb closure profiles, and the same theory and approaches used in low-temperature thermochronometry are generally applicable to higher temperature systems. The widely used low- to medium-temperature thermochronometric systems are reviewed in detail in these chapters, but while there are numerous chapters reviewing various aspects of the apatite (U-Th)/He system, there is no chapter singularly devoted to it, partly because of several previous reviews recently published on this topic.

The Shimanto Belt, Southwest Japan

The Shimanto Belt, Southwest Japan PDF Author: Asahiko Taira
Publisher: Gordon & Breach Science Pub
ISBN: 9780677256801
Category : Science
Languages : en
Pages : 542

Book Description
Detailed investigations of trench and forearc geological processes, the processes that operate in the early stages of mountain formation and are fundamental to crustal evolution of continents. Integrated studies of such processes should lead to a comprehensive modelling and full understanding of forearc-trench geodynamic phenomena. The Southwest Japan forearc region is one of the best areas to establish a good representative field study. This volume is a compilation of recent research results of the geotechnic framework and structural evolution of the region. The overview of Southwest Japan's geology is very extensive and could be used as base for comparative studies with other convergent margins or further detailed research in this region. The following topics are addressed: regional geology and tectonic synthesis, geochemistry, metamorphism and physical properties, forearc basin sedimentation, marine geology and geophysics, neogene evolution. Book club price, $206.00. Annotation copyrighted by Book News, Inc., Portland, OR

Geology and Tectonics of Subduction Zones: A Tribute to Gaku Kimura

Geology and Tectonics of Subduction Zones: A Tribute to Gaku Kimura PDF Author: Timothy Byrne
Publisher: Geological Society of America
ISBN: 0813725348
Category : Science
Languages : en
Pages : 215

Book Description
This volume highlights the career of Dr. Gaku Kimura, professor emeritus of geosciences at the University of Tokyo, by showing the spectrum of research required to understand these dynamic environments and the range of research he has inspired. The first three chapters provide context for the growth of accretionary prisms by examining the thermal structure of the ocean crust, and the sedimentary facies and potential fluid pathways in the Shikoku Basin. Next, two chapters look at the regional-scale structure of the plate boundary and the rheology and hysteresis of the hanging wall of the subduction zone in SW Japan. The following five chapters discuss the progressive deformation and thermal maturation of sediments along accretionary margins from Japan to New Zealand to western North America. The final two chapters look at the deformation processes near the subducting plate interface with the last chapter proposing a link between outcrop-scale observations and seismic slip.

Proceedings of the Ocean Drilling Program

Proceedings of the Ocean Drilling Program PDF Author: Ocean Drilling Program
Publisher:
ISBN:
Category : Borings
Languages : en
Pages : 786

Book Description


Ocean Drilling Program Proceedings

Ocean Drilling Program Proceedings PDF Author: Ocean Drilling Program
Publisher:
ISBN:
Category : Borings
Languages : en
Pages : 122

Book Description


Earth Accretionary Systems in Space and Time

Earth Accretionary Systems in Space and Time PDF Author: Peter Anthony Cawood
Publisher: Geological Society of London
ISBN: 9781862392786
Category : Science
Languages : en
Pages : 430

Book Description
Accretionary orogens form at convergent plate boundaries and include the supra-subduction zone forearc, magmatic arc and backarc components. They can be broken into retreating and advancing types, based on their kinematic framework and resulting geological character.Accretionary systems have been active throughout Earth history, extending back until at least 3.2 Ga, and provide an important constraint on the initiation of horizontal motion of lithospheric plates on Earth. Accretionary orogens have been responsible for major growth of the continental lithosphere, through the addition of juvenile magmatic products, but are also major sites of consumption and reworking of continental crust through time.The aim of this volume is to provide a better understanding of accretionary processes and their role in the formation and evolution of the continental crust. Fourteen papers deal with general aspects of accretion and metamorphism and discuss examples of accretionary orogens and crustal growth through Earth history, from the Archaean to the Cenozoic.