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Titlebook: Subduction Zone Geodynamics; Serge Lallemand,Francesca Funiciello Conference proceedings 2009 Springer-Verlag Berlin Heidelberg 2009 earth

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书目名称Subduction Zone Geodynamics
编辑Serge Lallemand,Francesca Funiciello
视频video
概述Covers most recent developments in subduction zone dynamics
丛书名称Frontiers in Earth Sciences
图书封面Titlebook: Subduction Zone Geodynamics;  Serge Lallemand,Francesca Funiciello Conference proceedings 2009 Springer-Verlag Berlin Heidelberg 2009 earth
描述.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
出版日期Conference proceedings 2009
关键词earthquake; geodynamics; oceanic; petrology; seismic; seismogenic; seismology; subduction; subduction zones;
版次1
doihttps://doi.org/10.1007/978-3-540-87974-9
isbn_softcover978-3-642-09973-1
isbn_ebook978-3-540-87974-9Series ISSN 1863-4621 Series E-ISSN 1863-463X
issn_series 1863-4621
copyrightSpringer-Verlag Berlin Heidelberg 2009
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Subduction with Variations in Slab Buoyancy: Models and Application to the Banda and Apennine System to ̃20 mm/year for the Apennine Arc. Increases in model slab dip and decreases in arc-trench distance are likewise consistent with hypocenter locations and volcanic arc position along the Banda and Sunda arcs. In contrast, a time period of ̃10 m.y. is needed for model subduction rates to slow to ne
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Continental Collision and the STEP-wise Evolution of Convergent Plate Boundaries: From Structure to f tear or STEP (Subduction-Transform-Edge-Propagator) faults are key elements. A STEP fault laterally decouples subducting lithosphere from non-subducting litho-sphere in a scissor type of fashion. It enhances the ability of a slab to retreat through the mantle fl ow around the edge of the subducted
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Imaging Interseismic Locking at the Nankai Subduction Zone, Southwest Japanrtical, rather than, horizontal, velocities because the vertical deformation fi eld will enable us to separate rigid plate motions from deformation due to interplate locking; horizontal displacements contain both rigid plate motion and deformation from interplate locking, whereas vertical displaceme
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