Experimental Evidence Supporting an Overturned Iron‐Titanium‐Rich Melt Layer in the Deep Lunar Interior-Reference-Cited by-同舟云学术

Experimental Evidence Supporting an Overturned Iron‐Titanium‐Rich Melt Layer in the Deep Lunar Interior

Published:2022-06-30 Issue:13 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Xu Man¹²^ORCID,Jing Zhicheng³^ORCID,Van Orman James A.²^ORCID,Yu Tony¹^ORCID,Wang Yanbin¹

Affiliation:

1. Center for Advanced Radiation Sources The University of Chicago Chicago IL USA

2. Department of Earth, Environmental, and Planetary Sciences Case Western Reserve University Cleveland OH USA

3. Department of Earth and Space Sciences Southern University of Science and Technology Shenzhen China

Funder

National Natural Science Foundation of China

National Science Foundation

U.S. Department of Energy

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL099066

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5. Buoyancy‐driven melt segregation in the Earth’s Moon, I. Numerical results;Delano J. W.;Proceedings of 20th lunar and planetary science conference,1990

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