Subduction Zone Geodynamics

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...

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Bibliographic Details
Other Authors: Lallemand, Serge (Editor), Funiciello, Francesca (Editor)
Format: eBook
Language:English
Published: Berlin, Heidelberg Springer Berlin Heidelberg 2009, 2009
Edition:1st ed. 2009
Series:Frontiers in Earth Sciences
Subjects:
Online Access:
Collection: Springer eBooks 2005- - Collection details see MPG.ReNa
Table of Contents:
  • Subduction Zone Geodynamics
  • A Review of the Role of Subduction Dynamics for Regional and Global Plate Motions
  • Subduction with Variations in Slab Buoyancy: Models and Application to the Banda and Apennine Systems
  • Continental Collision and the STEP-wise Evolution of Convergent Plate Boundaries: From Structure to Dynamics
  • Seismic Tomography and Anisotropy
  • Seismic Anisotropy of Subduction Zone Minerals–Contribution of Hydrous Phases
  • Local Earthquake Tomography in the Southern Tyrrhenian Region of Italy: Geophysical and Petrological Inferences on the Subducting Lithosphere
  • Great Subduction Zone Earthquakes
  • Effect of Subducting Seafloor Topography on the Rupture Characteristics of Great Subduction Zone Earthquakes
  • Great Earthquakes in Slow-Subduction, Low-Taper Margins
  • Seismogenic Zone Characterization
  • Convergent Margin Structure in High-Quality Geophysical Images and Current Kinematic and Dynamic Models
  • Imaging Interseismic Locking at the Nankai Subduction Zone, Southwest Japan
  • Continental and Ridge Subduction Processes
  • Exhumation Processes in Oceanic and Continental Subduction Contexts: A Review
  • Evolution of Subductions Indicated by Mélanges in Taiwan
  • Subduction of an Active Spreading Ridge Beneath Southern South America: A Review of the Cenozoic Geological Records from the Andean Foreland, Central Patagonia (46–47°S)
  • Configuration of the Colombian Caribbean Margin: Constraints from 2D Seismic Reflection data and Potential Fields Interpretation