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Subduction Zones And Back Arc Basins


Subduction Zones And Back Arc Basins
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Subduction Zones And Back Arc Basins


Subduction Zones And Back Arc Basins
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Author : M. Reyners
language : en
Publisher:
Release Date :

Subduction Zones And Back Arc Basins written by M. Reyners and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on with categories.




Subduction Zones And Back Arc Basins


Subduction Zones And Back Arc Basins
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Author : M. Reyners
language : en
Publisher:
Release Date : 1996

Subduction Zones And Back Arc Basins written by M. Reyners and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 1996 with Basins (Geology) categories.




Special Issue


Special Issue
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Author : International Association of Seismology and Physics of the Earth's Interior. General Assembly
language : en
Publisher:
Release Date : 1996

Special Issue written by International Association of Seismology and Physics of the Earth's Interior. General Assembly and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 1996 with Basins (Geology) categories.




Subduction Zones Part Ii


Subduction Zones Part Ii
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Author : Larry J. Ruff
language : en
Publisher: Birkhäuser
Release Date : 2012-12-06

Subduction Zones Part Ii written by Larry J. Ruff and has been published by Birkhäuser this book supported file pdf, txt, epub, kindle and other format this book has been release on 2012-12-06 with Science categories.


Subduction zones consume oceanic lithosphere and are an indispensible part of plate tectonics. Unlike the oceanic lithosphere production system which can be linked as a nearly continuous, albeit sinuous, strand around the earth, subduction zones are a rather dissociated group and are found in several isolated corners of the world. While plate tectonics can predict that subduction zones are required along certain plate boundaries, it does not stipulate how subduction zones initiate and develop. The preservation of newly created oceanic lithosphere and the propensity for spreading centers to fragment continents leaves a wealth of geological informa tion on the initiation and evolution of spreading. On the other hand, the subject of subduction initiation has little observational basis. To find such observations, we need to look at some muddled tectonic regimes. The Macquarie Ridge complex presents a natural laboratory for studies of subduction initiation. 2. Tectonics of the Macquarie Ridge Complex The Macquarie Ridge complex is a complicated physiographic feature that trends approximately north-south between South Island, New Zealand and the Pacific-Antarctica spreading center. This feature consists of a sequence of troughs and ridges, with Macquarie Island as the only exposed expression. The seismically active Macquarie Ridge complex (hereafter: MRC) is crudely continuous with the Tonga-Kermadec-New Zealand seismic activity. The basic physiographic features and seismicity of the MRC are shown in Figure I. The earthquake epicenters generally cluster about the bathymetric expression of the MRC.



Subduction Zones


Subduction Zones
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Author : Larry J. Ruff
language : en
Publisher:
Release Date : 1989

Subduction Zones written by Larry J. Ruff and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 1989 with Plate tectonics categories.




Subduction


Subduction
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Author : Alexander I. Shemenda
language : en
Publisher: Springer Science & Business Media
Release Date : 2012-12-06

Subduction written by Alexander I. Shemenda and has been published by Springer Science & Business Media this book supported file pdf, txt, epub, kindle and other format this book has been release on 2012-12-06 with Science categories.


This book is devoted to the quantitative physical modeling of subduction and subduction-related processes. It presents a coherent description of the modeling method (including similarity criteria, and a novel applied experimental technique), results from model experiments, theoretical analysis of results on the basis of continuum mechanics, and their geodynamic interpretation. Subduction is modeled in general as well as applied to particular regions using both 2-D and 3-D approaches, with both slab-push and slab-pull driving forces. The modeling covers all stages from subduction initiation to `death', different regimes of subduction producing back arc extension and compression, blocking of subduction and jumps of subduction zone, arc-continent collision and continental subduction. This work is for geologists and geophysicists interested in geodynamics of the convergent plate boundaries and in mechanics of the lithosphere.



Island Arcs Deep Sea Trenches And Back Arc Basins


Island Arcs Deep Sea Trenches And Back Arc Basins
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Author : Manik Talwani
language : en
Publisher: American Geophysical Union
Release Date : 1977

Island Arcs Deep Sea Trenches And Back Arc Basins written by Manik Talwani and has been published by American Geophysical Union this book supported file pdf, txt, epub, kindle and other format this book has been release on 1977 with Science categories.


Proceedings of a symposium held in honor of Maurice Ewing at Arden House, Harriman, N.Y. on March 28-31, 1976.



Intra Oceanic Subduction Systems


Intra Oceanic Subduction Systems
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Author : Robert D. Larter
language : en
Publisher: Geological Society of London
Release Date : 2003

Intra Oceanic Subduction Systems written by Robert D. Larter and has been published by Geological Society of London this book supported file pdf, txt, epub, kindle and other format this book has been release on 2003 with Science categories.


Recycling of oceanic plate back into the Earth's interior at subduction zones is one of the key processes in Earth evolution. Volcanic arcs, which form above subduction zones, are the most visible manifestations of plate tectonics, the convection mechanism by which the Earth loses excess heat. They are probably also the main location where new continental crust is formed, the so-called 'subduction factory' About 400f modern subduction zones on Earth are intra-oceanic. These subduction systems are generally simpler than those at continental margins as they commonly have a shorter history of subduction and their magmas are not contaminated by ancient sialic crust. They are therefore the optimum locations for studies of mantle processes and magmatic addition to the crust in subduction zones.



Subduction Zone Geodynamics


Subduction Zone Geodynamics
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Author : Serge Lallemand
language : en
Publisher: Springer Science & Business Media
Release Date : 2009-02-11

Subduction Zone Geodynamics written by Serge Lallemand and has been published by Springer Science & Business Media this book supported file pdf, txt, epub, kindle and other format this book has been release on 2009-02-11 with Science categories.


Subduction is a major process that plays a first-order role in the dynamics of the Earth. The sinking of cold lithosphere into the mantle is thought by many authors to be the most important source of energy for plates driving forces. It also deeply modifies the thermal and chemical structure of the mantle, producing arc volcanism and is responsible for the release of most of the seismic energy on Earth. There has been considerable achievements done during the past decades regarding the complex interactions between the various processes acting in subduction zones. This volume contains a collection of contributions that were presented in June 2007 in Montpellier (France) during a conference that gave a state of the art panorama and discussed the perspectives about "Subduction Zone Geodynamics". The papers included in this special volume offer a unique multidisciplinary picture of the recent research on subduction zones geodynamics. They are organized into five main topics: Subduction zone geodynamics, Seismic tomography and anisotropy, Great subduction zone earthquakes, Seismogenic zone characterization, Continental and ridge subduction processes. Each of the 13 papers collected in the present volume is primarily concerned with one of these topics. However, it is important to highlight that papers always treat more than one topic so that all are related lighting on different aspects of the complex and fascinating subduction zones geodynamics.



Arc Continent Collision


Arc Continent Collision
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Author : Dennis Brown
language : en
Publisher: Springer Science & Business Media
Release Date : 2011-06-29

Arc Continent Collision written by Dennis Brown and has been published by Springer Science & Business Media this book supported file pdf, txt, epub, kindle and other format this book has been release on 2011-06-29 with Science categories.


Arc-continent collision has been one of the important tectonic processes in the formation of mountain belts throughout geological time, and it continues to be so today along tectonically active plate boundaries such as those in the SW Pacific or the Caribbean. Arc-continent collision is thought to have been one of the most important process involved in the growth of the continental crust over geological time, and may also play an important role in its recycling back into the mantle via subduction. Understanding the geological processes that take place during arc-continent collision is therefore of importance for our understanding of how collisional orogens evolve and how the continental crust grows or is destroyed. Furthermore, zones of arc-continent collision are producers of much of the worlds primary economic wealth in the form of minerals, so understanding the processes that take place during these tectonic events is of importance in modeling how this mineral wealth is formed and preserved. This book brings together seventeen papers that are dedicated to the investigation of the tectonic processes that take place during arc-continent collision. It is divided into four sections that deal firstly with the main players involved in any arc-continent collision; the continental margin, the subduction zone, and finally the volcanic arc and its mineral deposits. The second section presents eight examples of arc-continent collisions that range from being currently active through to Palaeoproterozoic in age. The third section contains two papers, one that deals with the obduction of large-slab ophiolites and a second that presents a wide range of physical models of arc-continent collision. The fourth section brings everything that comes before together into a discussion of the processes of arc-continent collision.