特提斯喜马拉雅错那洞穹隆的岩石组合、构造特征与成因

张林奎; 张志; 李光明; 董随亮; 夏祥标; 梁维; 付健刚; 曹华文

doi:10.3799/dqkx.2018.141

Volume 43 Issue 8

Aug. 2018

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Article Navigation > Earth Science > 2018 > 43(8): 2664-2683

Zhang Linkui, Zhang Zhi, Li Guangming, Dong Suiliang, Xia Xiangbiao, Liang Wei, Fu Jiangang, Cao Huawen, 2018. Rock Assemblage, Structural Characteristics and Genesis Mechanism of the Cuonadong Dome, Tethys Himalaya. Earth Science, 43(8): 2664-2683. doi: 10.3799/dqkx.2018.141

Citation:

Zhang Linkui, Zhang Zhi, Li Guangming, Dong Suiliang, Xia Xiangbiao, Liang Wei, Fu Jiangang, Cao Huawen, 2018. Rock Assemblage, Structural Characteristics and Genesis Mechanism of the Cuonadong Dome, Tethys Himalaya. Earth Science, 43(8): 2664-2683. doi: 10.3799/dqkx.2018.141

Citation:

Zhang Linkui, Zhang Zhi, Li Guangming, Dong Suiliang, Xia Xiangbiao, Liang Wei, Fu Jiangang, Cao Huawen, 2018. Rock Assemblage, Structural Characteristics and Genesis Mechanism of the Cuonadong Dome, Tethys Himalaya. Earth Science, 43(8): 2664-2683. doi: 10.3799/dqkx.2018.141

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Rock Assemblage, Structural Characteristics and Genesis Mechanism of the Cuonadong Dome, Tethys Himalaya

doi: 10.3799/dqkx.2018.141

Chengdu Center of China Geological Survey, Chengdu 610081, China

Received Date: 2018-03-10
Publish Date: 2018-08-15

Abstract

Abstract

The structure assemblage, rock composition, and kinematics characteristics of metamorphic deformation of the newly discovered Cuonadong dome are not clear currently, which seriously hinders the restoration of its evolutionary process and the anatomy of the coupled relationship between the formation of plutonium and mineralization. Based on the detailed field geological survey, the newly discovered magmatic rocks in dome were additionally collected for chronological study in this paper. The results show that the Cuonadong dome is divided into three structural layers of upper (margin)-middle (mantle)-lower (core) by upper and lower detachment faults. The core rock assemblages are primarily composed of granite gneiss, leucogranite, and a little migmatite, with a large amount of intruded pegmatite veins. The mantle rock assemblage is a set of strongly metamorphic and deformable schist with interlayer carbonate. This rock assemblage has Barrovian metamorphism confirmed by mineral assemblages from the core to the margin of kyanite+staurolite+garnet+biotite→taurolite+garnet+biotite→garnet+cordierite+biotite→chlorite+biotite; The margin is primarily comprised of slightly metamorphic Triassic-Jurassic sedimentary rocks, which is constituted of sericite chlorite sand slate and a small amount of phyllite. The dome from early to late has experienced N-S trending thrusting, N-S extension and E-W extension, and the formation of the dome is primarily associated with the N-S extension. There are five episodes of magmatism in the dome at ~500 Ma (gneiss), 140 Ma (diabase), 26 Ma (deformed two-mica granite/pegmatite), 18 Ma (weakly oriented two-mica granite), 16.8-15.9 Ma (garnet-tourmaline-bearing granite). The study shows that the formation of the Cuonadong dome is the result of the combined effect of the early extension and detachment and the late magmatic diapir, and the movement of the South Tibetan detachment system during the Eocene-Oligocene is the primal factor.
- Cuonadong dome,
- structure assemblage,
- metamorphic zoning,
- Tethys Himalayan,
- zircon U-Pb dating,
- geochemistry,
- structural geology

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References(74)

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