Mantle dynamics inferred from the crystallographic preferred orientation of bridgmanite

Noriyoshi Tsujino (), Yu Nishihara, Daisuke Yamazaki, Yusuke Seto, Yuji Higo and Eiichi Takahashi
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Noriyoshi Tsujino: Institute for Planetary Materials, Okayama University
Yu Nishihara: Geodynamics Research Center, Ehime-University
Daisuke Yamazaki: Institute for Planetary Materials, Okayama University
Yusuke Seto: Kobe University
Yuji Higo: Japan Synchrotron Radiation Research Institute
Eiichi Takahashi: Tokyo Institute of Technology

Nature, 2016, vol. 539, issue 7627, 81-84

Abstract: Deformation experiments on bridgmanite indicate that it may be the main contributor to the shear wave anisotropy observed around several subducting plates.

Date: 2016
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DOI: 10.1038/nature19777

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