globalchange  > 气候减缓与适应
DOI: 10.1002/2014GL061954
论文题名:
High-pressure melting of MgO from (Mg,Fe)O solid solutions
作者: Du Z.; Lee K.K.M.
刊名: Geophysical Research Letters
ISSN: 0094-9591
EISSN: 1944-9322
出版年: 2014
卷: 41, 期:22
起始页码: 8061
结束页码: 8066
语种: 英语
英文关键词: ferropericlase ; high pressure melting ; magnesium oxide
Scopus关键词: Earth (planet) ; Experimental mineralogy ; High pressure engineering ; Magnesium ; Melting ; Planets ; Ab initio prediction ; Core-mantle boundary ; Earth's mantle ; Ferropericlase ; High pressure melting ; High temperature behavior ; Laser-heated diamond anvil cells ; Planetary interiors ; Magnesia ; experimental study ; high pressure ; high temperature ; mantle ; melting ; oxide ; prediction ; solar system ; temperature effect
英文摘要: Magnesium oxide (MgO) is a significant component of planetary interiors, particularly Earth's mantle and other rocky planets within and beyond our solar system; thus its high-pressure, high-temperature behavior is important to understanding the thermochemical evolution of planets. Laser-heated diamond-anvil cell (DAC) experiments on (Mg,Fe)O ferropericlase up to ~40 GPa show that previous DAC experiments on MgO melting are too low, while previous multi-anvil experiments yield melting temperatures too high. Instead, our quasi-static experimental results are consistent with recent ab initio predictions as well as dynamic shock measurements. Extrapolated to the core-mantle boundary (CMB) of the Earth, MgO is expected to melt at ~8000 ± 500 K, much greater than expected geotherm temperatures. © 2014. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84923368535&doi=10.1002%2f2014GL061954&partnerID=40&md5=8ce4e7618d56bad44f34333f8a810af5
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/6855
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作者单位: Department of Geology and Geophysics, Yale University, New Haven, CT, United States

Recommended Citation:
Du Z.,Lee K.K.M.. High-pressure melting of MgO from (Mg,Fe)O solid solutions[J]. Geophysical Research Letters,2014-01-01,41(22).
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