Fluid‐Induced Fault Reactivation Due To Brucite + Antigorite Dehydration Triggered the Mw7.1 September 19th Puebla‐Morelos (Mexico) Intermediate‐Depth Earthquake-Reference-Cited by-同舟云学术

Fluid‐Induced Fault Reactivation Due To Brucite + Antigorite Dehydration Triggered the Mw7.1 September 19th Puebla‐Morelos (Mexico) Intermediate‐Depth Earthquake

Published:2022-10-26 Issue:20 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Gutiérrez‐Aguilar F.¹^ORCID,Hernández‐Uribe D.²³^ORCID,Holder R. M.³^ORCID,Condit C. B.⁴^ORCID

Affiliation:

1. Facultad de Ingeniería Universidad Nacional Autónoma de México Ciudad de México México

2. Department of Earth and Environmental Sciences University of Illinois Chicago IL USA

3. Department of Earth and Environmental Sciences University of Michigan Ann Arbor MI USA

4. Earth and Space Sciences Department University of Washington Seattle WA USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL100814

Reference67 articles.

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

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3. Permeability of subducted oceanic crust revealed by eclogite-facies vugs

4. Seawater-peridotite interactions: First insights from ODP Leg 209, MAR 15°N

5. Watching Dehydration: Seismic Indication for Transient Fluid Pathways in the Oceanic Mantle of the Subducting Nazca Slab

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