Intermediate‐Depth Earthquakes Controlled by Incoming Plate Hydration Along Bending‐Related Faults-Reference-Cited by-同舟云学术

Intermediate‐Depth Earthquakes Controlled by Incoming Plate Hydration Along Bending‐Related Faults

Published:2019-04-04 Issue:7 Volume:46 Page:3688-3697
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Boneh Yuval¹²^ORCID,Schottenfels Emily³^ORCID,Kwong Kevin⁴,Zelst Iris⁵^ORCID,Tong Xinyue⁶,Eimer Melody⁷,Miller Meghan S.⁸^ORCID,Moresi Louis⁹^ORCID,Warren Jessica M.¹⁰^ORCID,Wiens Douglas A.⁷^ORCID,Billen Magali¹¹^ORCID,Naliboff John¹¹,Zhan Zhongwen¹²^ORCID

Affiliation:

1. Department of Geological SciencesBrown University Providence RI USA

2. Now at Department of Geological and Environmental SciencesBen‐Gurion University of the Negev Be'er‐Sheva Israel

3. Department of Earth and EnvironmentBoston University Boston MA USA

4. Roy M. Huffington Department of Earth ScienceSouthern Methodist University Dallas TX USA

5. Seismology and Wave PhysicsInstitute of Geophysics, Department of Earth Sciences, ETH Zürich Zürich Switzerland

6. Department of Geological Sciences, Jackson School of GeosciencesUniversity of Texas at Austin Austin TX USA

7. Department of Earth and Planetary SciencesWashington University in St. Louis Saint Louis MO USA

8. Research School of Earth SciencesAustralian National University Canberra ACT Australia

9. School of Earth SciencesUniversity of Melbourne Parkville Victoria Australia

10. Department of Geological SciencesUniversity of Delaware Newark DE USA

11. Department of GeologyUniversity of California Davis CA USA

12. Seismological Laboratory, Division of Geological and Planetary SciencesCalifornia Institute of Technology Pasadena CA USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL081585

Reference100 articles.

1. Hydrated subducted crust at 100–250 km depth

2. Thermal–petrological controls on the location of earthquakes within subducting plates

3. Dynamic control on serpentine crystallization in veins: Constraints on hydration processes in oceanic peridotites

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

5. The relationship of intermediate- and deep-focus seismicity to the hydration and dehydration of subducting slabs

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