Faulting within the Pacific plate at the Mariana Trench: Implications for plate interface coupling and subduction of hydrous minerals-Reference-Cited by-同舟云学术

Faulting within the Pacific plate at the Mariana Trench: Implications for plate interface coupling and subduction of hydrous minerals

Published:2014-04 Issue:4 Volume:119 Page:3076-3095
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Emry Erica L.¹²,Wiens Douglas A.²,Garcia‐Castellanos Daniel³

Affiliation:

1. Now at Department of Geosciences Pennsylvania State University University Park Pennsylvania USA

2. Department of Earth and Planetary Sciences Washington University St. Louis Missouri USA

3. Instituto de Ciencias de la Tierra Jaume Almera, CSIC Barcelona Spain

Funder

NSF

NSF/FESD CIDER

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2013JB010718

Reference98 articles.

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3. Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing

4. Barklage M.(2010) Structure and seismicity of the upper mantle using deployments of broadband seismographs in Antarctica and the Mariana Islands PhD dissertation 115 pp Washington University in Saint Louis Saint Louis.

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