Nanophase Iron Particles Derived From Fayalitic Olivine Decomposition in Chang'E‐5 Lunar Soil: Implications for Thermal Effects During Impacts-Reference-Cited by-同舟云学术

Nanophase Iron Particles Derived From Fayalitic Olivine Decomposition in Chang'E‐5 Lunar Soil: Implications for Thermal Effects During Impacts

Author:

Guo Zhuang¹²,Li Chen¹³,Li Yang¹⁴^ORCID,Wen Yuanyun¹,Tai Kairui¹⁵,Li Xiongyao¹⁴,Liu Jianzhong¹⁴^ORCID,Ouyang Ziyuan¹

Affiliation:

1. Center for Lunar and Planetary Sciences Institute of Geochemistry Chinese Academy of Sciences Guiyang China

2. College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China

3. Faculty of Metallurgical and Energy Engineering Kunming University of Science and Technology Kunming China

4. Center for Excellence in Comparative Planetology Chinese Academy of Sciences Hefei China

5. Department of Geology Northwest University Xi'an China

Funder

National Natural Science Foundation of China

Youth Innovation Promotion Association

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

Reference39 articles.

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