中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Crustal remelting origin of highly silicic magmatism on the Moon

文献类型:期刊论文

作者Su, Bin3; Chen, Yi3,4; Yue, Zongyu1; Chen, Lin3; Mitchell, Ross N.3,4; Tang, Ming2; Yang, Wei1; Huang, Guangyu3; Guo, Jinghui3; Li, Xian-Hua3
刊名COMMUNICATIONS EARTH & ENVIRONMENT
出版日期2023-06-28
卷号4期号:1页码:9
DOI10.1038/s43247-023-00900-8
英文摘要Partial remelting of KREEP - potassium, rare earth element, phosphorus - basalts on the moon, could explain the occurrence of highly silicic magmatism, which on Earth requires water and plate tectonics, according to phase equilibrium simulations Orbital observations of non-mare, highly silicic volcanic constructs on the Moon challenge the conventional view of the formation of silicic crusts in the presence of water and plate tectonics-the former the Moon has in very short supply and the latter it likely never ever had. Revealing the silica-rich magma origin may reshape our understanding of early planetary crust formation. However, the cause of lunar silicic magmatism remains enigmatic. Here we conduct phase equilibrium simulations for potential lunar igneous lithologies that demonstrate that the compositions of silicic volcanic constructs can be produced by partial melting of KREEP (potassium, rare earth elements, and phosphorus) basalts. Either internal radiogenic heating or external impact bombardment can provide the heat needed for KREEP basalt melting. Combined with silica-rich materials identified on other rocky planets, we suggest that highly evolved crusts might be more prevalent in the early solar system than anticipated as they can originate from crustal remelting in the absence of water and plate tectonics.
WOS关键词CONTINENTAL-CRUST ; HYDROCODE SIMULATION ; LUNAR ; IMPACT ; VOLCANISM ; EVOLUTION ; WATER ; PETROLOGY ; GEOCHEMISTRY ; DEFORMATION
资助项目National Natural Science Foundation of China[42272057] ; Key Research Program of the Chinese Academy of Sciences[ZDBS-SSW-JSC007-15] ; Institute of Geology and Geophysics, Chinese Academy of Sciences[IGGCAS-202101]
WOS研究方向Environmental Sciences & Ecology ; Geology ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:001020925600001
出版者SPRINGERNATURE
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Key Research Program of the Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/111256]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
地质与地球物理研究所_中国科学院地球与行星物理重点实验室
通讯作者Chen, Yi
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
2.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Su, Bin,Chen, Yi,Yue, Zongyu,et al. Crustal remelting origin of highly silicic magmatism on the Moon[J]. COMMUNICATIONS EARTH & ENVIRONMENT,2023,4(1):9.
APA Su, Bin.,Chen, Yi.,Yue, Zongyu.,Chen, Lin.,Mitchell, Ross N..,...&Wu, Fu-Yuan.(2023).Crustal remelting origin of highly silicic magmatism on the Moon.COMMUNICATIONS EARTH & ENVIRONMENT,4(1),9.
MLA Su, Bin,et al."Crustal remelting origin of highly silicic magmatism on the Moon".COMMUNICATIONS EARTH & ENVIRONMENT 4.1(2023):9.

入库方式: OAI收割

来源:地质与地球物理研究所

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