Equation of State for Shocked Fe‐8.6 wt% Si up to 240 GPa and 4,670 K-Reference-Cited by-同舟云学术

Equation of State for Shocked Fe‐8.6 wt% Si up to 240 GPa and 4,670 K

Author:

Huang Haijun¹^ORCID,Leng Chunwei¹,Wang Qingsong²,Young Gang¹^ORCID,Liu Xun¹,Wu Ye¹^ORCID,Xu Feng¹^ORCID,Fei Yingwei³

Affiliation:

1. School of Sciences Wuhan University of Technology Wuhan China

2. National Key Laboratory of Shock Wave and Detonation Physics, Institute of Fluid Physics China Academy of Engineering Physics Mianyang China

3. Geophysical Laboratory Carnegie Institution of Washington Washington DC USA

Funder

Fundamental Research Funds for the Central Universities

National Natural Science Foundation of China

National Basic Research Program of China

Publisher

American Geophysical Union (AGU)

Subject

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

Link

Reference56 articles.

1. The chemical composition of the Earth;Allègre C. J.;Earth and Planetary Science Letters,1995

2. Additive equation of state for silicates at high pressures;Al'tshuler L. V.;Izvestiya Akademii Nauk SSR, Fizicheskaya Zemli,1971

Cited by 17 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Earth's core composition and core formation;Reference Module in Earth Systems and Environmental Sciences;2024