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No large earthquakes in fully exposed subducted seamount

Published:2019-03-06 Issue:5 Volume:47 Page:407-410
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:

Author:

Bonnet G.¹,Agard P.¹,Angiboust S.²,Fournier M.¹,Omrani J.³

Affiliation:

1. Sorbonne Université, CNRS-INSU, Institut des Sciences de la Terre de Paris, ISTeP UMR 7193, CNRS F-75005 Paris, France

2. Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, CNRS, F-75005 Paris, France

3. Geological Survey of Iran, Tehran, Iran

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/geology/article-pdf/47/5/407/4680705/407.pdf

Reference32 articles.

1. Zagros orogeny: A subduction-dominated process;Agard;Geological Magazine,2011

2. The subduction plate interface: Rock record and mechanical coupling (from long to short timescales);Agard;Lithos,2018

3. Zagros blueschists: Episodic underplating and long-lived cooling of a subduction zone;Angiboust;Earth and Planetary Science Letters,2016

4. Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing;Audet;Nature,2009

5. Pseudotachylytes from Corsica: Fossil earthquakes from a subduction complex;Austrheim;Terra Nova,2004

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