Accretionary prisms in subduction earthquake cycles: The theory of dynamic Coulomb wedge

Author:

Wang Kelin12,Hu Yan2

Affiliation:

1. Pacific Geoscience Centre; Geological Survey of Canada; Sidney, British Columbia Canada

2. School of Earth and Ocean Sciences; University of Victoria; Victoria, British Columbia Canada

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference75 articles.

1. Crustal dynamics and active fault mechanics during subduction erosion: Application of frictional wedge analysis on to the North Chilean Forearc;Adam;Tectonophysics,2000

2. Source mechanisms and tectonic significance of historical earthquakes along the Nankai Trough;Ando;Tectonophysics,1975

3. Structure and deformational history of the inner forearc region, Hikurangi subduction margin, New Zealand;Beanland;N. Z. J. Geol. Geophys.,1998

4. The CORK experiment in Hole 949C: Long-term observations of pressure and temperature in the Barbados accretionary prism;Becker;Proc. Ocean Drill. Program Sci. Results,1997

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