Formation of bridgmanite-enriched layer at the top lower-mantle during magma ocean solidification

Journal: Nature Communications

Published: 2020-01-28

DOI: 10.1038/s41467-019-14071-8

Affiliations: 5

Authors: 10

Go to article
Institutions Share
Synchrotron SOLEIL, France 0.30
Institute for Planetary Materials, Okayama University, Japan 0.25
Laboratory of Magma and Volcanism (LMV), France 0.20
Japan Synchrotron Radiation Research Institute (JASRI), Japan 0.20
Bavarian Research Institute of Experimental Geochemistry and Geophysics (BGI), UBT, Germany 0.05

Return

Except where otherwise noted © 2021 Springer Nature Limited. All Rights Reserved.
partner of AGORA, HINARI, OARE, INASP, ORCID, CrossRef and COUNTER