Shock Compression and Melting of an Fe-Ni-Si Alloy: Implications for the Temperature Profile of the Earth's Core and the Heat Flux Across the Core-Mantle Boundary

Author:

Zhang Youjun12ORCID,Sekine Toshimori12,Lin Jung-Fu13ORCID,He Hongliang4,Liu Fusheng5,Zhang Mingjian5,Sato Tomoko2,Zhu Wenjun4,Yu Yin4

Affiliation:

1. Center for High Pressure Science and Technology Advanced Research (HPSTAR); Shanghai China

2. Department of Earth and Planetary Systems Science; Hiroshima University; Higashihiroshima Japan

3. Department of Geological Sciences, Jackson School of Geosciences; The University of Texas at Austin; Austin TX USA

4. National Key Laboratory of Shock Wave and Detonation Physics; China Academy of Engineering Physics; Mianyang China

5. College of Physical Science and Technology; Southwest Jiaotong University; Chengdu China

Funder

NSF Geophysics Program and Deep Carbon Observatory of the Sloan Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference110 articles.

1. Melting-induced stratification above the Earth's inner core due to convective translation;Alboussiere;Nature,2010

2. Iron under Earth's core conditions: Liquid-state thermodynamics and high-pressure melting curve from ab initio calculations;Alfè;Physical Review B,2002

3. The chemical composition of the Earth;Allègre;Earth and Planetary Science Letters,1995

4. The Earth's core and the phase diagram of iron;Anderson;Philosophical Transactions of the Royal Society of London A: Mathematical, Physical and Engineering Sciences,1982

5. Solidus and liquidus profiles of chondritic mantle: Implication for melting of the Earth across its history;Andrault;Earth and Planetary Science Letters,2011

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