Massive sediment accretion at ∼80 km depth along the subduction interface: Evidence from the southern Chinese Tianshan-Reference-Cited by-同舟云学术

Massive sediment accretion at ∼80 km depth along the subduction interface: Evidence from the southern Chinese Tianshan

Published:2018-04-06 Issue:6 Volume:46 Page:495-498
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:

Author:

Bayet Léa¹,John Timm¹,Agard Philippe²,Gao Jun³,Li Ji-Lei³

Affiliation:

1. Institut für Geologische Wissenschaften, Freie Universität Berlin, Malteserstrasse 74–100, 12449 Berlin, Germany

2. ISTEP, UMR CNRS 7193, UPMC Sorbonne Universités, F-75005 Paris, France

3. Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/geology/article-pdf/46/6/495/4180238/495.pdf

Reference30 articles.

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2. The thermal structure of subduction zones constrained by seismic imaging: Implications for slab dehydration and wedge flow;Abers;Earth and Planetary Science Letters,2006

3. Exhumation of oceanic blueschists and eclogites in subduction zones: Timing and mechanisms;Agard;Earth-Science Reviews,2009

4. QuIB Calc: A MATLAB® script for geobarometry based on Raman spectroscopy and elastic modeling of quartz inclusions in garnet;Ashley;Computers & Geosciences,2014

5. Diapirs as the source of the sediment signature in arc lavas;Behn;Nature Geoscience,2011

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