Plume‐Induced Breakup of a Subducting Plate: Microcontinent Formation Without Cessation of the Subduction Process-Reference-Cited by-同舟云学术

Plume‐Induced Breakup of a Subducting Plate: Microcontinent Formation Without Cessation of the Subduction Process

Published:2019-04-02 Issue:7 Volume:46 Page:3663-3675
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Koptev Alexander¹²^ORCID,Beniest Anouk³^ORCID,Gerya Taras⁴^ORCID,Ehlers Todd A.¹^ORCID,Jolivet Laurent²^ORCID,Leroy Sylvie²^ORCID

Affiliation:

1. Department of GeosciencesUniversity of Tübingen Tübingen Germany

2. Institut des Sciences de la Terre de Paris (ISTeP)Sorbonne Université, CNRS Paris France

3. Department of Earth SciencesVrije Universiteit Amsterdam Amsterdam The Netherlands

4. ETH‐Zurich, Institute of Geophysics Zurich Switzerland

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL081295

Reference99 articles.

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3. Zagros orogeny: a subduction-dominated process

4. Barrier E. Vrielynck B. Brouillet J. F. &Brunet M. F.(2018).Paleotectonic reconstruction of the Central Tethyan Realm. Tectono‐sedimentary‐palinspastic maps from Late Permian to Pliocene.Atlas of 20 maps (scale: 1/15 000 000) CCGM/CGMW.http://www.ccgm.org.

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