期刊
PHYSICS OF THE EARTH AND PLANETARY INTERIORS
卷 185, 期 3-4, 页码 107-111出版社
ELSEVIER SCIENCE BV
DOI: 10.1016/j.pepi.2011.02.004
关键词
XANES; Silicate perovskite; Ferropericlase; Fe-Mg partitioning; Diamond anvil cell; In situ laser heating
资金
- National Science Foundation - Earth Sciences [EAR-0622171]
- Department of Energy-Geosciences [DE-FG02-94ER14466]
- U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences [DE-AC02-06CH11357]
- Eurocores EuroMinSci Programme
- German Science Foundation (DFG) [SPP1236, Mc 3/16-1, Mc 3/16-2]
- Stifterverband far die Deutsche Wissenchaft
The effect of spin crossover in lower mantle silicate perovskite (Pv) and ferropericlase (Fp) on the iron partitioning between these two phases remains uncertain, mainly due to the lack of in situ experiments under the relevant pressure and temperature conditions. By combining in situ synchrotron X-ray absorption and diffraction measurements on synthetic ringwoodite and natural (Mg(0.88)Fe(0.12))(2)SiO(4) San Carlos olivine at pressures between 22 GPa and 115 GPa treated at temperatures of 1950-2300 K, we found that temperature promotes iron partitioning into Pv, while pressure acts oppositely. There is only a limited effect of spin crossover in co-existing Pv and Fp on iron partitioning which cannot produce an appreciable chemical inhomogeneity within the Earth's lower mantle spin transition zone. Crown Copyright (C) 2011 Published by Elsevier B.V. All rights reserved.
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