Garnet fracturing reveals ancient unstable slip events hosted in plate interface metasediments-Reference-Cited by-同舟云学术

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Garnet fracturing reveals ancient unstable slip events hosted in plate interface metasediments

Published:2024-08 Issue: Volume:640 Page:118794
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Angiboust Samuel^ORCID,Ioannidi Paraskevi Io^ORCID,Muldashev Iskander^ORCID

Publisher

Elsevier BV

Reference71 articles.

1. The rise and demise of deep accretionary wedges: a long-term field and numerical modeling perspective;Angiboust;Geosphere,2022

2. A 100-my-long window onto mass-flow processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile);Angiboust;GSA Bull.,2018

3. Probing the transition between seismically coupled and decoupled segments along an ancient subduction interface;Angiboust;Geochem. Geophys. Geosyst.,2015

4. Eclogite breccias in a subducted ophiolite: a record of intermediate-depth earthquakes?;Angiboust;Geology,2012

5. Subcritical crack growth in geological materials;Atkinson;J. Geophys. Res.: Solid Earth,1984

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