Slab temperature controls on the Tonga double seismic zone and slab mantle dehydration-Reference-Cited by-同舟云学术

Slab temperature controls on the Tonga double seismic zone and slab mantle dehydration

Author:

Wei S. Shawn¹²^ORCID,Wiens Douglas A.¹,van Keken Peter E.³^ORCID,Cai Chen¹^ORCID

Affiliation:

1. Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA.

2. Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA.

3. Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC 20015, USA.

Abstract

The Tonga double seismic zone depth and distribution are controlled by slab temperature, which affects dehydration reactions.

Funder

Division of Ocean Sciences

Division of Earth Sciences

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference54 articles.

1. On the two-layered structure of deep seismic plane in northeastern Japan arc;Umino N.;J. Seismol. Soc. Jpn.,1975

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