Two-billion-year-old volcanism on the Moon from Chang’e-5 basalts

The Moon has a magmatic and thermal history that is distinct from that of the terrestrial planets(1). Radioisotope dating of lunar samples suggests that most lunar basaltic magmatism ceased by around 2.9–2.8 billion years ago (Ga)(2,3), although younger basalts between 3 Ga and 1 Ga have been sugges...

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Detalles Bibliográficos
Autores principales: Li, Qiu-Li, Zhou, Qin, Liu, Yu, Xiao, Zhiyong, Lin, Yangting, Li, Jin-Hua, Ma, Hong-Xia, Tang, Guo-Qiang, Guo, Shun, Tang, Xu, Yuan, Jiang-Yan, Li, Jiao, Wu, Fu-Yuan, Ouyang, Ziyuan, Li, Chunlai, Li, Xian-Hua
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8636262/
https://www.ncbi.nlm.nih.gov/pubmed/34666338
http://dx.doi.org/10.1038/s41586-021-04100-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8636262/
https://www.ncbi.nlm.nih.gov/pubmed/34666338
http://dx.doi.org/10.1038/s41586-021-04100-2

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