Fusible mantle cumulates trigger young mare volcanism on the cooling Moon

The Chang’E-5 (CE5) mission has demonstrated that lunar volcanism was still active until two billion years ago, much younger than the previous isotopically dated lunar basalts. How the small Moon retained enough heat to drive such late volcanism is unknown, particularly as the CE5 mantle source was...

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Detalles Bibliográficos
Autores principales: Su, Bin, Yuan, Jiangyan, Chen, Yi, Yang, Wei, Mitchell, Ross N., Hui, Hejiu, Wang, Hao, Tian, Hengci, Li, Xian-Hua, Wu, Fu-Yuan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2022
Materias:
Earth, Environmental, Ecological, and Space Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9586486/
https://www.ncbi.nlm.nih.gov/pubmed/36269823
http://dx.doi.org/10.1126/sciadv.abn2103

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9586486/
https://www.ncbi.nlm.nih.gov/pubmed/36269823
http://dx.doi.org/10.1126/sciadv.abn2103

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