中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Olivine-norite rock detected by the lunar rover Yutu-2 likely crystallized from the SPA-impact melt pool

文献类型:期刊论文

作者Lin, Honglei9; He, Zhiping10; Yang, Wei9; Lin, Yangting9; Xu, Rui10; Zhang, Chi9; Zhu, Meng-Hua2; Chang, Rui9; Zhang, Jin-Hai9; Li, Chunlai10
刊名NATIONAL SCIENCE REVIEW
出版日期2020-05-01
卷号7期号:5页码:913-920
ISSN号2095-5138
关键词impact basin lunar interior composition visible and near-infrared spectra lunar rover Yutu-2 Chang'E-4 mission
DOI10.1093/nsr/nwz183
英文摘要Chang'E-4 landed in the South Pole-Aitken (SPA) basin, providing a unique chance to probe the composition of the lunar interior. Its landing site is located on ejecta strips in Von Karman crater that possibly originate from the neighboring Finsen crater. A surface rock and the lunar regolith at 10 sites along the rover Yutu-2 track were measured by the onboard Visible and Near-Infrared Imaging Spectrometer in the first three lunar days of mission operations. In situ spectra of the regolith have peak band positions at 1 and 2 mu m, similar to the spectral data of Finsen ejecta from the Moon Mineralogy Mapper, which confirms that the regolith's composition of the landing area is mostly similar to that of Finsen ejecta. The rock spectrum shows similar band peak positions, but stronger absorptions, suggesting relatively fresh exposure. The rock may consist of 38.1 +/- 5.4% low-Ca pyroxene, 13.9 +/- 5.1% olivine and 48.0 +/- 3.1% plagioclase, referred to as olivine-norite. The plagioclase-abundant and olivine-poor modal composition of the rock is inconsistent with the origin of the mantle, but representative of the lunar lower crust. Alternatively, the rock crystallized from the impact-derived melt pool formed by the SPA-impact event via mixing the lunar crust and mantle materials. This scenario is consistent with fast-cooling thermal conditions of a shallow melt pool, indicated by the fine to medium-sized texture (<3 mm) of the rock and the SPA-impact melting model [Icarus 2012; 220: 730-43].
WOS关键词POLE-AITKEN BASIN ; CHANGE-4 LANDING SITE ; IMAGING SPECTROMETER ; PHOTOMETRIC CORRECTION ; SURFACE ; DIFFERENTIATION ; IDENTIFICATION ; MINERALOGY ; PYROXENES ; SPECTRA
资助项目Key Research Program of Frontier Sciences, Chinese Academy of Sciences[QYZDJSSW-DQC001] ; National Natural Science Foundation of China[41902318] ; National Natural Science Foundation of China[41490631] ; National Natural Science Foundation of China[41525016] ; National Natural Science Foundation of China[11941001] ; Beijing Municipal Science and Technology Commission[Z181100002918003]
WOS研究方向Science & Technology - Other Topics
语种英语
出版者OXFORD UNIV PRESS
WOS记录号WOS:000537524500011
资助机构Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, 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 ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, 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 ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, 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 ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, 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 ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission ; Beijing Municipal Science and Technology Commission
源URL[http://ir.iggcas.ac.cn/handle/132A11/96634]  
专题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Lin, Yangting
作者单位1.Shandong Univ, Inst Space Sci, Shandong Prov Ke Lab Opt Astron & Solar Terr Envi, Weihai 264209, Peoples R China
2.Macau Univ Sci & Technol, State Key Lab Lunar & Planetary Sci, Macau, Peoples R China
3.Beijing Inst Space Mech & Elect, Beijing 100076, Peoples R China
4.Chinese Acad Sci, Natl Space Sci Ctr, State Key Lab Space Weather, Beijing 100190, Peoples R China
5.Chinese Acad Sci, State Key Lab Remote Sensing Sci, Inst Remote Sensing & Digital Earth, Beijing 100101, Peoples R China
6.Chinese Acad Sci, Natl Space Sci Ctr, Key Lab Elect & Informat Technol Space Syst, Beijing 100190, Peoples R China
7.Chinese Acad Sci, Xian Inst Opt & Precis Mech, Xian 710119, Peoples R China
8.Chinese Acad Sci, Inst Opt & Elect, Chengdu 610209, Peoples R China
9.Chinese Acad Sci, Key Lab Earth & Planetary Phys, Inst Geol & Geophys, Beijing 100029, Peoples R China
10.Chinese Acad Sci, Shanghai Inst Tech Phys, Key Lab Space Act Optoelect Technol, Shanghai 200083, Peoples R China
推荐引用方式
GB/T 7714
Lin, Honglei,He, Zhiping,Yang, Wei,et al. Olivine-norite rock detected by the lunar rover Yutu-2 likely crystallized from the SPA-impact melt pool[J]. NATIONAL SCIENCE REVIEW,2020,7(5):913-920.
APA Lin, Honglei.,He, Zhiping.,Yang, Wei.,Lin, Yangting.,Xu, Rui.,...&Zou, Yongliao.(2020).Olivine-norite rock detected by the lunar rover Yutu-2 likely crystallized from the SPA-impact melt pool.NATIONAL SCIENCE REVIEW,7(5),913-920.
MLA Lin, Honglei,et al."Olivine-norite rock detected by the lunar rover Yutu-2 likely crystallized from the SPA-impact melt pool".NATIONAL SCIENCE REVIEW 7.5(2020):913-920.

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来源:地质与地球物理研究所

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