Compositional mantle layering revealed by slab stagnation at ~1000-km depth

Author:

Ballmer Maxim D.12,Schmerr Nicholas C.3ORCID,Nakagawa Takashi4ORCID,Ritsema Jeroen5ORCID

Affiliation:

1. Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo 152-8551, Japan.

2. School of Ocean and Earth Sciences and Technology, University of Hawaii at Manoa, Honolulu, HI 96822, USA.

3. Department of Geology, University of Maryland, College Park, MD 20742, USA.

4. Department of Mathematical Science and Advanced Technology, Japan Agency for Marine-Earth Science and Technology, Yokohama 236-0001, Japan.

5. Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109, USA.

Abstract

The stagnation of ~1000-km deep slabs indicates that dense basalt may be more abundant in the lower mantle than in the upper mantle.

Funder

National Science Foundation

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference96 articles.

1. A. E. Ringwood Origin of the Earth and Moon (Springer Berlin Germany 1979).

2. Major and trace element composition of the depleted MORB mantle (DMM)

3. A perovskitic lower mantle inferred from high-pressure, high-temperature sound velocity data;Murakami M.;Nature,2012

4. BurnMan: A lower mantle mineral physics toolkit

5. Thermochemical interpretation of 1-D seismic data for the lower mantle: The significance of nonadiabatic thermal gradients and compositional heterogeneity;Cobden L.;J. Geophys. Res.,2009

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