Reconciliation of the negative pressure dependence of the 660-km discontinuity depth with the bridgmanite forming reactions in MgO-SiO<SUB>2</SUB> systems

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    LI["Linked Institutions (3)"]
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ADS bibcode
2020AGUFMDI0050020C
year
2020
Listed Authors
Chanyshev, A.
Ishii, T.
Bondar, D.
Bhat, S.
Kim, E. J.
Farla, R. J.
Liu, Z.
Wang, L.
Nakajima, A.
Yang, B.
Tang, H.
Chen, Z.
Higo, Y.
Tange, Y.
Katsura, T.
Listed Institutions
Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
University of Bayreuth, Bayerisches Geoinstitut, Bayreuth, Germany
Deutsche Elektronen-Synchrotron (DESY), Hamburg, Germany
University of Bayreuth, Bayerisches Geoinstitut, Bayreuth, Germany
Deutsche Elektronen-Synchrotron (DESY), Hamburg, Germany
Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
University of Bayreuth, Bayerisches Geoinstitut, Bayreuth, Germany
Tohoku University, Sendai, Japan
Center for High Pressure Science and Technology Advanced Research, Beijing, China
Center for High Pressure Science and Technology Advanced Research, Beijing, China
Center for High Pressure Science and Technology Advanced Research, Beijing, China
Japan Synchrotron Radiation Research Institute, Hyogo, Japan
Japan Synchrotron Radiation Research Institute, Hyogo, Japan
Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany

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