中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Impact history and origin of lunar meteorite Northwest Africa 15528

文献类型:期刊论文

作者Liu, Runchuan4,5,6; He, Huaiyu4,5,6; Smith, Thomas4,5,6; Ye, Hanqing4,5,6; Wang, Huapei1; Zhang, Xuhang4,5,6; Su, Fei4,5,6; Liu, Ziheng4,5,6; Guo, Wei4,5,6; Yang, Peng2
刊名SCIENCE CHINA-EARTH SCIENCES
出版日期2023-05-17
页码24
关键词The Moon Regolith Meteorites Cosmic rays Solar wind Thermal histories Far side of the Moon
ISSN号1674-7313
DOI10.1007/s11430-022-1049-4
英文摘要No samples from the Moon's far side have been returned to Earth. Thus, lunar meteorite study can deepen the understanding of the Moon's far side (if we can identify which lunar meteorites came from the Moon's far side). The Northwest Africa (NWA) 15528 meteorite is a lunar feldspathic regolith breccia meteorite and we speculated it might originate from the Feldspathic Highlands Terrane (FHT) on the far side of the Moon. Here, we report detailed petrography, major and trace elements, and noble gas (He, Ne, and Ar) isotopes for the clasts and matrix, respectively. The results show that the NWA 15528 lunar meteorite contains diverse clasts, including anorthosite, granulite, basalt, and impact melt clasts. The coarse, well-crystallized, uniform chemical composition minerals may come from intrusive plutonic rocks. Among the anorthosite clasts, the norite/olivine clasts originate from the deep lunar crust, whereas the other anorthosite clasts are from lunar highlands. The Sm concentrations in NWA 15528 were similar to those in the fourth group of Apollo 16 melt samples, demonstrating that NWA 15528 has a typical plagioclase highland meteorite composition. Compared with the Apollo sample data and remote sensing results, the chemical composition of NWA 15528 indicated strong affinities with the FHT area and ferroan anorthosite (FAN) material from the far side of the Moon. The noble gas isotopic composition of NWA 15528 is consistent with a binary mixture of solar wind and cosmogenic components; during stepwise pyrolytic extractions, we observed that the abundance of cosmogenic components decreased, whereas that of solar wind components increased with increasing temperature. The average cosmic-ray exposure (CRE) age of the matrix and granulite is 42 +/- 6 Ma, with a shielding depth in the same range of 10-20 g cm(-2). The gas retention age of NWA 15528 is 2.14 Ga, and the antiquity age of NWA 15528 is (0.69-0.74)+/- 0.2 Ga (considering 50% Ar-40(m) is Ar-40(trap)) which indicates the different clasts of NWA 15528 are assembled after 0.69-0.74 Ga.
WOS关键词ALEXANDRA RANGE 93069 ; LA-ICP-MS ; NOBLE-GASES ; ISOTOPIC COMPOSITION ; REGOLITH BRECCIAS ; IN-SITU ; GEOCHEMISTRY ; AGES ; HIGHLANDS ; EVOLUTION
资助项目Strategic Priority Program B of the Chinese Academy of Sciences[XDB41010205] ; Civil Aerospace Pre-Research Project[D020302] ; Strategic Priority Program A of the Chinese Academy of Sciences[XDA17010403] ; Strategic Priority Program A of the Chinese Academy of Sciences[XDB41010304] ; National Natural Science Foundation of China[42030205] ; National Natural Science Foundation of China[41874079]
WOS研究方向Geology
语种英语
WOS记录号WOS:000993376500001
出版者SCIENCE PRESS
资助机构Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the 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 ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the 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 ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the 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 ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Strategic Priority Program B of the Chinese Academy of Sciences ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Civil Aerospace Pre-Research Project ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the Chinese Academy of Sciences ; Strategic Priority Program A of the 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
源URL[http://ir.iggcas.ac.cn/handle/132A11/110963]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者He, Huaiyu; Smith, Thomas
作者单位1.China Univ Geosci, Sch Geophys & Geomatics, Paleomagnetism & Planetary Magnetism Lab, Wuhan 430074, Peoples R China
2.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China
3.Guilin Univ Technol, Inst Meteorites, Planetary Mat Res Ctr, Guilin 541004, Peoples R China
4.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
6.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Liu, Runchuan,He, Huaiyu,Smith, Thomas,et al. Impact history and origin of lunar meteorite Northwest Africa 15528[J]. SCIENCE CHINA-EARTH SCIENCES,2023:24.
APA Liu, Runchuan.,He, Huaiyu.,Smith, Thomas.,Ye, Hanqing.,Wang, Huapei.,...&Lu, Chao.(2023).Impact history and origin of lunar meteorite Northwest Africa 15528.SCIENCE CHINA-EARTH SCIENCES,24.
MLA Liu, Runchuan,et al."Impact history and origin of lunar meteorite Northwest Africa 15528".SCIENCE CHINA-EARTH SCIENCES (2023):24.

入库方式: OAI收割

来源:地质与地球物理研究所

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