月球虹湾-雨海盆地壳幔结构

王旭媛; 梁青; 陈超; 杜劲松; 张双喜

doi:10.3799/dqkx.2015.141

Volume 40 Issue 9

Sep. 2015

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Article Navigation > Earth Science > 2015 > 40(9): 1566-1575

Wang Xuyuan, Liang Qing, Chen Chao, Du Jinsong, Zhang Shuangxi, 2015. Crust-Mantle Structure beneath the Sinus Iridum- Mare Imbrium Basin of the Moon. Earth Science, 40(9): 1566-1575. doi: 10.3799/dqkx.2015.141

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Wang Xuyuan, Liang Qing, Chen Chao, Du Jinsong, Zhang Shuangxi, 2015. Crust-Mantle Structure beneath the Sinus Iridum- Mare Imbrium Basin of the Moon. Earth Science, 40(9): 1566-1575. doi: 10.3799/dqkx.2015.141

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Crust-Mantle Structure beneath the Sinus Iridum- Mare Imbrium Basin of the Moon

doi: 10.3799/dqkx.2015.141

Wang Xuyuan^1
,,
Liang Qing^{1, 2
,
,},
Chen Chao^{1, 2},
Du Jinsong¹,
Zhang Shuangxi¹

1.
Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, China
2.
Hubei Subsurface Multi-scale Imaging Key Laboratory, China University of Geosciences, Wuhan 430074, China

Received Date: 2015-03-20
Publish Date: 2015-09-15

Abstract

Abstract

In order to investigate the material migration of crust and mantle after the formation of large impact basins, a study on the undulation of crust-mantle interface, using new lunar gravity data is carried out. This has an important significance for the research of the formation and evolution of impact basin. The forward modeling of the gravity anomaly established by filling mare basalts in Sinus Iridum-Mare Imbrium basin area shows that the gravity anomaly only accounts for about 8% in the amplitude of total Bouguer gravity anomaly, while the rest 92% is mainly related to the perturbation of crust-mantle interface. The edge detection of the Bouguer gravity anomaly at different observing heights in Sinus Iridum-Mare Imbrium area indicates that the crust-mantle interface beneath the area of Sinus Iridum-Mare Imbrium northwest leans to the center of Mare Imbrium with increasing depth. It is concluded that extra mantle uplifts to Sinus Iridum area in the crust-mantle interface may have been caused by the impact forming Mare Imbrium basin. This or the later Sinus Iridum impact may have induced a second effect on the crust-mantle structure beneath Mare Imbrium basin. During the lunar mantle rebounds, there may have been a force dragging the mantle beneath the Mare Imbrium toward the Sinus Iridum area.
- Moon,
- Sinus Iridum-Mare Imbrium area,
- crust-mantle structure,
- gravity,
- edge detection

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References(43)

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Crust-Mantle Structure beneath the Sinus Iridum- Mare Imbrium Basin of the Moon

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