Geometry and Width of the Ringwoodite – Bridgmanite+Ferropericlase Binary Loop in the System (Mg,Fe)2SiO4: Interpretation of the Sharpness of the 660-km Discontinuity
Tomoo Katsura1, Takayuki Ishii2, Rong Huang2, Fumiya Maeda3, Liang Yuan3, Shrikant Bhat4, Robert J Farla4, Takaaki Kawazoe5, Noriyoshi Tsujino6, Zhaodong Liu7, Hongzhan Fei8, Lin Wang2, Dmitry Druzhbin7, Takafumi Yamamoto9, Eleonora Kulik10, Iuliia Koemets7, Yuji Higo11 and Yoshinori Tange12, (1)University Bayreuth, Bayerisches Geoinstitut, Bayreuth, Germany, (2)University of Bayreuth, Bayerisches Geoinstitut, Bayreuth, Germany, (3)Tohoku University, Sendai, Japan, (4)Deutsche Elektronen-Synchrotron (DESY), Hamburg, Germany, (5)Bayerisches Geoinstitut, Universitaet Bayreuth, Bayreuth, Germany, (6)Japan Synchrotron Radiation Research Institute, Hyogo, Japan, (7)University of Bayreuth, Bayreuth, Germany, (8)Zhejiang University, School of Earth Sciences, Hangzhou, China, (9)Hiroshima University, Higashi-Hiroshima, Japan, (10)DESY, Hamburg, Germany, (11)Japan Synchrotron Radiation Research Institute, Kouto, Japan, (12)Ehime University, Ehime, Japan
