High-pressure phase transitions of Fe3-xTixO4 solid solution up to 60 GPa correlated with electronic spin transition

American Mineralogist - Tập 98 Số 4 - Trang 736-744 - 2013
T. Yamanaka1, Atsushi Kyono2,1, Yuki Nakamoto3,1, Yu Meng4, S. A. Kharlamova5, Viktor V. Struzhkin1, Yanming Ma1,4,6
1Geophysical Laboratory, Carnegie Institution of Washington. Washington, D.C. 20015, U.S.A.
2Division of Earth Evolution Sciences, Graduate School of Life and Environment Sciences, University of Tsukuba, Tsukuba 3058-572, Japan
3Center of Quantum Science and Technology under Extreme Conditions Osaka University, Osaka 560-8531, Japan
4High Pressure Collaborative Access Team, Geophysical Laboratory, Carnegie Institution of Washington, Argonne, Illinois 60439, U.S.A.
5High Pressure Synergetic Consortium, Geophysical Laboratory, Carnegie Institution of Washington, Argonne, Illinois 60439, U.S.A. High Pressure Synergetic Consortium, Geophysical Laboratory, Carnegie Institution of Washington, Argonne, Illinois 60439, U.S.A.
6High Pressure Synergetic Consortium, Geophysical Laboratory, Carnegie Institution of Washington, Argonne, Illinois 60439, U.S.A.

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American Mineralogist

Tập 98 Số 4

736-744

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