Seismic visibility of a deep subduction channel – insights from numerical simulation of high-frequency seismic waves emitted from intermediate depth earthquakes

Return flow in a deep subduction channel (DSC) has been proposed to explain rapid exhumation of high pressure–low temperature metamorphic rocks, entirely based on the fossil rock record. Supported by thermo-mechanical models, the DSC is envisioned as a thin layer on top of the subducted plate reachi...

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Bibliographic Details
Main Authors: W. Friederich, L. Lambrecht, B. Stöckhert, S. Wassmann, C. Moos
Format: Article
Language:English
Published: Copernicus Publications 2014-03-01
Series:Solid Earth
Online Access:http://www.solid-earth.net/5/141/2014/se-5-141-2014.pdf