Three-dimensional finite-element models on the deformation of forearcs caused by aseismic ridge subduction: The role of ridge shape, friction coefficient of the plate interface and mechanical properties of the forearc-Reference-Cited by-同舟云学术

Three-dimensional finite-element models on the deformation of forearcs caused by aseismic ridge subduction: The role of ridge shape, friction coefficient of the plate interface and mechanical properties of the forearc

Published:2016-08 Issue: Volume:684 Page:76-91
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Zeumann Stefanie,Hampel Andrea

Funder

Deutsche Forschungsgemeinschaft

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference72 articles.

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3. Global bathymetry and elevation data at 30 arc seconds resolution: SRTM30_PLUS;Becker;Mar. Geod.,2009

4. Subduction of Atlantic aseismic ridges and Late Cenozoic evolution of the Lesser Antilles island arc;Bouysse;Tectonophysics,1990

5. A modelling study of vertical surface displacements at convergent plate margins;Buiter;Geophys. J. Int.,2001

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