Olivine-norite rock detected by the lunar rover Yutu-2 likely crystallized from the SPA-impact melt pool

Chang’E-4 landed in the South Pole-Aitken (SPA) basin, providing a unique chance to probe the composition of the lunar interior. Its landing site is located on ejecta strips in Von Kármán crater that possibly originate from the neighboring Finsen crater. A surface rock and the lunar regolith at 10 s...

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Detalles Bibliográficos
Autores principales: Lin, Honglei, He, Zhiping, Yang, Wei, Lin, Yangting, Xu, Rui, Zhang, Chi, Zhu, Meng-Hua, Chang, Rui, Zhang, Jinhai, Li, Chunlai, Lin, Hongyu, Liu, Yang, Gou, Sheng, Wei, Yong, Hu, Sen, Xue, Changbin, Yang, Jianfeng, Zhong, Jie, Fu, Xiaohui, Wan, Weixing, Zou, Yongliao
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Oxford University Press 2020
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288882/
https://www.ncbi.nlm.nih.gov/pubmed/34692112
http://dx.doi.org/10.1093/nsr/nwz183

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288882/
https://www.ncbi.nlm.nih.gov/pubmed/34692112
http://dx.doi.org/10.1093/nsr/nwz183

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