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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...
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 |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2021
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Materias: | |
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 |
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