多龙矿集区色那东岩体年龄、成因与动力学背景

王勤; 林彬; 唐菊兴; 宋扬; 李彦波; 侯俊富; 李玉彬; 卫鲁杰

doi:10.3799/dqkx.2017.613

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1125-1141

Wang Qin, Lin Bin, Tang Juxing, Song Yang, Li Yanbo, Hou Junfu, Li Yubin, Wei Lujie, 2018. Diagenesis, Lithogenesis and Geodynamic Setting of Intrusions in Senadong Area, Duolong District, Tibet. Earth Science, 43(4): 1125-1141. doi: 10.3799/dqkx.2017.613

Citation:

Wang Qin, Lin Bin, Tang Juxing, Song Yang, Li Yanbo, Hou Junfu, Li Yubin, Wei Lujie, 2018. Diagenesis, Lithogenesis and Geodynamic Setting of Intrusions in Senadong Area, Duolong District, Tibet. Earth Science, 43(4): 1125-1141. doi: 10.3799/dqkx.2017.613

Citation:

Wang Qin, Lin Bin, Tang Juxing, Song Yang, Li Yanbo, Hou Junfu, Li Yubin, Wei Lujie, 2018. Diagenesis, Lithogenesis and Geodynamic Setting of Intrusions in Senadong Area, Duolong District, Tibet. Earth Science, 43(4): 1125-1141. doi: 10.3799/dqkx.2017.613

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Diagenesis, Lithogenesis and Geodynamic Setting of Intrusions in Senadong Area, Duolong District, Tibet

doi: 10.3799/dqkx.2017.613

Wang Qin^{1,2
,},
Lin Bin²,
Tang Juxing^{2
,
,},
Song Yang²,
Li Yanbo³,
Hou Junfu⁴,
Li Yubin¹,
Wei Lujie³

1.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Key Laboratory of Metallogeny and Mineral Resources Assessment of Ministry of Land and Resources, Beijing 100037, China
3.
No.5 Geological Party, Tibet Bureau of Geology and Exploration, Golmud 816000, China
4.
Chinalco Tibet Mining Co., Ltd., Lhasa 850000, China

Received Date: 2017-12-18
Publish Date: 2018-04-15

Abstract

Abstract

Duolong district has more than 20 million tons of copper resources, which is the top large-scale Cu-Au mineral district in China. However, the prospecting potential in its peripheral region is still huge. This paper reports the geochronology and geochemical test results of the granite porphyry and diorite porphyry in the Senadong area for the first time, providing data for regional metallogenic regularity. In this study, the accurate zircon isotopic dating, Hf isotopic and whole rock major and trace elements reveal that emplacement ages of granitic and dioritic porphyries 123±2 Ma, respectively; the formation of rocks is related to partial melting of subducted oceanic plate, and the magma contains significant mantle source component. Based on these results, it is proposed that the intrusions of the Senadong area adjacent to ore-bearing porphyry in Duolong district formed during the period of the Early Cretaceous magmatic activity, suggesting that they possibly have the same geodynamic background. All these intrusions are the products of Bangongco-Nujiang ocean arc-arc "soft" collision, which occurred in the end of subduction transform to the beginning of the collision. These magmas provide heat and fluid for mineralization, which suggests that the Senadong area could be a potential district to find the new porphyry deposits.
- U-Pb dating of zircon,
- petrology,
- geochemistry,
- Hf isotope,
- Senadong,
- Tibet

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References(121)

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