Stagnant Slab: A Review-Reference-Cited by-同舟云学术

Stagnant Slab: A Review

Published:2009-05-01 Issue:1 Volume:37 Page:19-46
ISSN:0084-6597
Container-title:Annual Review of Earth and Planetary Sciences
language:en
Short-container-title:Annu. Rev. Earth Planet. Sci.

Author:

Fukao Yoshio¹,Obayashi Masayuki¹,Nakakuki Tomoeki²,

Affiliation:

1. Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushimacho, Yokosuka, 237-0061, Japan;

2. Department of Earth and Planetary Systems Sciences, Graduate School of Science, Hiroshima University, 1-3-1 Kagamiyama, Higashi-Hiroshima, 739-8526, Japan;

Abstract

A stagnant slab is a subducted slab of oceanic lithosphere subhorizontally deflected above, across, or below the 660 km discontinuity. This phenomenon has now been widely recognized beneath subduction zones around the circum-Pacific and in the Mediterranean. Collaboration of seismic and electromagnetic observations, mineral physics measurements, and geodynamic modeling has begun to provide a consistent picture of stagnant slab.

Publisher

Annual Reviews

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Astronomy and Astrophysics

Link

https://www.annualreviews.org/doi/pdf/10.1146/annurev.earth.36.031207.124224

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