东昆仑西段阿确墩地区晚古生代花岗岩成因、锆石U-Pb年龄及其地质意义

李猛; 胡朝斌; 查显锋; 高晓峰; 李婷; 姚志亮

doi:10.3799/dqkx.2020.162

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2598-2609

Li Meng, Hu Chaobin, Zha Xianfeng, Gao Xiaofeng, Li Ting, Yao Zhiliang, 2020. Genesis, Zircon U-Pb Geochronology and Geological Significance of Late Paleozoic Granite in Aquedun, West of East Kunlun Mountains. Earth Science, 45(7): 2598-2609. doi: 10.3799/dqkx.2020.162

Citation:

Li Meng, Hu Chaobin, Zha Xianfeng, Gao Xiaofeng, Li Ting, Yao Zhiliang, 2020. Genesis, Zircon U-Pb Geochronology and Geological Significance of Late Paleozoic Granite in Aquedun, West of East Kunlun Mountains. Earth Science, 45(7): 2598-2609. doi: 10.3799/dqkx.2020.162

Citation:

Li Meng, Hu Chaobin, Zha Xianfeng, Gao Xiaofeng, Li Ting, Yao Zhiliang, 2020. Genesis, Zircon U-Pb Geochronology and Geological Significance of Late Paleozoic Granite in Aquedun, West of East Kunlun Mountains. Earth Science, 45(7): 2598-2609. doi: 10.3799/dqkx.2020.162

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Genesis, Zircon U-Pb Geochronology and Geological Significance of Late Paleozoic Granite in Aquedun, West of East Kunlun Mountains

doi: 10.3799/dqkx.2020.162

Li Meng^{1, 2
,
,},
Hu Chaobin^{1, 2},
Zha Xianfeng^{1, 2},
Gao Xiaofeng^{1, 2},
Li Ting^{1, 2},
Yao Zhiliang³

1.
Xi'an Center of Geological Survey, CGS, Orogen Research Center of China Geological Survey, Xi'an 710054, China
2.
Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an 710054, China
3.
Xi'an Northwest Nonferrous Chemical Exploration Team Co. Ltd., Xi'an 710000, China

Received Date: 2020-06-19
Publish Date: 2020-07-15

Abstract

Abstract

The Late Paleozoic granitic rocks, which is batholith-like, in Aquedun, the west of East Kunlun mountains are mainly distributed in the area of Baozigou. The geochemical characteristics showed that it has calc-alkaline and weak peraluminous (A/CNK=0.99-1.04).The standardized distribution of chondrites of rare earth elements is steep on the left and slow on the right with negative Eu anomaly(δEu=0.73-0.97). Trace elements show losses of high-field strength elements such as Nb, Ta and Ti, which are believed to be formed in the continental margin arc environment and belong to the I-type granite. By the technique of LA-ICP-MS, zircon U-Pb dating of the granitic rock shows that the age of the monzonitic granite is 281.5±4.0 Ma. It is believed that the granite formed in the late of Early Permian. Combined with the regional tectonic evolution, it shows that the Paleotethys ocean began to subducting to the Tarim plate in the late of Early Permian, which may represent the earliest time of subduction, and the Paleotethys ocean was at the end of extension and the beginning of subduction transition.
- East Kunlun orogenic belt,
- monzonite granite,
- geochemistry,
- zircon U-Pb dating,
- Paleotethys ocean

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References(87)

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Genesis, Zircon U-Pb Geochronology and Geological Significance of Late Paleozoic Granite in Aquedun, West of East Kunlun Mountains

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