月球的撞击历史及其对月表物质的改造
Impact history of the Moon and its modification of lunar surface materials
查看参考文献116篇
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文摘
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外来天体物质的高速撞击作用贯穿了月球形成和演化的全部历史。撞击作用是塑造月球全球地貌、改造月表物质的物理化学特征、影响月球多圈层演化的重要地质营力。月球上的撞击过程、撞击历史及其对月表物质的改造,一直是月球科学研究的重要内容,也是月球探测的重点研究对象。本文综述了近十年来国、内外在月球的撞击过程、撞击历史和撞击改造浅表层物质研究中的重要进展,重点介绍了基于我国嫦娥探月工程获取的科学数据的相关研究成果,展望了该研究的发展方向,并对未来探测的重要观测目标提出了建议。 |
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其他语种文摘
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The high-speed impacts by celestial materials occurred throughout the full history of formation and evolution of the Moon. Impact cratering has been the dominating force in shaping the surface topography,modifying the physical and chemical characteristics of surface materials,and affecting various evolutionary aspects of the Moon. The process and history of impact cratering and its modification of lunar surface materials on the Moon have always been important research topics of the lunar science,and also the key scientific objects of all previous lunar explorations. In this work,we briefly summarized and reviewed some interesting and important advances in researches of impact processes and impact history on the Moon and shallow surface materials modified by the impact in the past ten years,particularly provided an overview of relevant research achievements based on the scientific data obtained by the Chang’E lunar exploration project,made prospects on future research directions of the lunar science,and proposed some suggestions on future exploring important observation targets and personal recommendations for the future development of disciplines of planetary science in China. |
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来源
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矿物岩石地球化学通报
,2023,42(3):462-477 【核心库】
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DOI
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10.19658/j.issn.1007-2802.2023.42.051
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关键词
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月球
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高速撞击
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撞击坑
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月壤
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撞击熔融
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高压相变
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地址
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1.
中山大学, 广东, 珠海, 519000
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中国科学院地质与地球物理研究所, 北京, 100029
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桂林理工大学, 广西, 桂林, 541006
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深圳大学, 广东, 深圳, 518060
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中国科学院地球化学研究所, 贵阳, 550081
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中国科学院空天信息创新研究院, 北京, 100094
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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1007-2802 |
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学科
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天文学;地质学 |
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基金
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国家自然科学基金
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文献收藏号
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CSCD:7522538
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参考文献 共
116
共6页
|
|
1.
Barrat J A. Lithium behavior during cooling of a dry basalt: An ion-microprobe study of the lunar meteorite Northwest Africa 479 (NWA 479).
Geochimica et Cosmochimica Acta,2005,69(23):5597-5609
|
CSCD被引
4
次
|
|
|
|
|
2.
Bottke W F. An Archaean heavy bombardment from a destabilized extension of the asteroid belt.
Nature,2012,485(7396):78-81
|
CSCD被引
11
次
|
|
|
|
|
3.
Bottke W F. The collisional evolution of the main asteroid belt.
Asteroids IV,2015:701-724
|
CSCD被引
1
次
|
|
|
|
|
4.
Bottke W F. The late heavy bombardment.
Annual Review of Earth and Planetary Sciences,2017,45:619-647
|
CSCD被引
16
次
|
|
|
|
|
5.
Bottke W F Jr. The Yarkovsky and Yorp effects: Implications for asteroid dynamics.
Annual Review of Earth And Planetary Sciences,2006,34:157-191
|
CSCD被引
11
次
|
|
|
|
|
6.
Brasser R. Impact bombardment chronology of the terrestrial planets from 4.5 Ga to 3.5 Ga.
Icarus,2020,338:113514
|
CSCD被引
2
次
|
|
|
|
|
7.
Chang Y R. An updated constraint on the local stratigraphy at the Chang'E-4 landing site.
Earth and Planetary Physics,2021,5(1):19-31
|
CSCD被引
3
次
|
|
|
|
|
8.
Chapman C R. What are the real constraints on the existence and magnitude of the late heavy bombardment?.
Icarus,2007,189(1):233-245
|
CSCD被引
2
次
|
|
|
|
|
9.
Cohen B A. Support for the lunar cataclysm hypothesis from lunar meteorite impact melt ages.
Science,2000,290(5497):1754-1756
|
CSCD被引
13
次
|
|
|
|
|
10.
De Sousa Ribeiro R. Dynamical evidence for an early giant planet instability.
Icarus,2020,339:113605
|
CSCD被引
1
次
|
|
|
|
|
11.
Ding C Y. A rocky hill on the continuous ejecta of Ziwei crater revealed by the Chang'e-3 mission.
Earth Planetary Physics,2020,4(2):105-110
|
CSCD被引
3
次
|
|
|
|
|
12.
Ding C Y. Layering structures in the porous material beneath the chang'e-3 landing site.
Earth and Space Science,2020,7(10):e2019EA000862
|
CSCD被引
3
次
|
|
|
|
|
13.
Ding C Y. Fragments delivered by secondary craters at the Chang'E-4 landing site.
Geophysical Research Letters,2020,47(7)
|
CSCD被引
6
次
|
|
|
|
|
14.
Ding C Y. Rock fragments in shallow lunar regolith: Constraints by the lunar penetrating radar onboard the Chang'E‐4 mission.
Journal of Geophysical Research: Planets,2021,126(9):e2021JE006917
|
CSCD被引
5
次
|
|
|
|
|
15.
Ding C. Compositional variations along the route of Chang'E-3 Yutu rover revealed by the lunar penetrating radar.
Progress in Earth,Planets and Space,2020,7(1):1-11
|
CSCD被引
1
次
|
|
|
|
|
16.
Ding C Y. A potential subsurface cavity in the continuous ejecta deposits of the Ziwei crater discovered by the Chang'E-3 mission.
Earth,Planets and Space,2021,73(1):53
|
CSCD被引
4
次
|
|
|
|
|
17.
Ding C Y. Yutu-2 radar observation of the lunar regolith heterogeneity at the Chang'E-4 landing site.
Astronomy & Astrophysics,2022,664:A43
|
CSCD被引
2
次
|
|
|
|
|
18.
Fa W Z. Regolith thickness over the lunar nearside: Results from Earth-based 70 cm Arecibo radar observations.
Icarus,2012,218(2):771-787
|
CSCD被引
24
次
|
|
|
|
|
19.
Fa W Z. Regolith thickness over Sinus Iridum: Results from morphology and size-frequency distribution of small impact craters.
Journal of Geophysical Research: Planets,2014,119(8):1914-1935
|
CSCD被引
5
次
|
|
|
|
|
20.
Fa W Z. Regolith stratigraphy at the Chang'E-3 landing site as seen by lunar penetrating radar.
Geophysical Research Letters,2015,42(23):10179-10187
|
CSCD被引
15
次
|
|
|
|
|
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