大兴安岭南段道伦达坝黑云母花岗岩成岩时代、锆石微量元素、Lu-Hf同位素特征及地质意义

李岩; 许立权; 李廷栋; 肖庆辉; 郭灵俊; 程杨; 范玉须; 庞进力; 袁伟明; 罗鹏跃

doi:10.3799/dqkx.2020.099

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2585-2597

Li Yan, Xu Liquan, Li Tingdong, Xiao Qinghui, Guo Lingjun, Cheng Yang, Fan Yuxu, Pang Jinli, Yuan Weiming, Luo Pengyue, 2020. Geochronology, Zircon Trace Element and Lu-Hf Isotope Characteristics of the Biotite Granite and Their Geological Significance from Daolundaba Cu Polymetallic Deposit, Southern Great Hinggan Ling, China. Earth Science, 45(7): 2585-2597. doi: 10.3799/dqkx.2020.099

Citation:

Li Yan, Xu Liquan, Li Tingdong, Xiao Qinghui, Guo Lingjun, Cheng Yang, Fan Yuxu, Pang Jinli, Yuan Weiming, Luo Pengyue, 2020. Geochronology, Zircon Trace Element and Lu-Hf Isotope Characteristics of the Biotite Granite and Their Geological Significance from Daolundaba Cu Polymetallic Deposit, Southern Great Hinggan Ling, China. Earth Science, 45(7): 2585-2597. doi: 10.3799/dqkx.2020.099

Citation:

Li Yan, Xu Liquan, Li Tingdong, Xiao Qinghui, Guo Lingjun, Cheng Yang, Fan Yuxu, Pang Jinli, Yuan Weiming, Luo Pengyue, 2020. Geochronology, Zircon Trace Element and Lu-Hf Isotope Characteristics of the Biotite Granite and Their Geological Significance from Daolundaba Cu Polymetallic Deposit, Southern Great Hinggan Ling, China. Earth Science, 45(7): 2585-2597. doi: 10.3799/dqkx.2020.099

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Geochronology, Zircon Trace Element and Lu-Hf Isotope Characteristics of the Biotite Granite and Their Geological Significance from Daolundaba Cu Polymetallic Deposit, Southern Great Hinggan Ling, China

doi: 10.3799/dqkx.2020.099

1.
Inner Mongolia Key Laboratory of Magmatic Mineralization and Ore-Prospecting, Hohhot 010020, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Institute of Mineral Research, China Metallurgical Geology Bureau, Beijing 101300, China
4.
General Prospecting Institute China National Administration of Coal Geology, Beijing 100039, China

Received Date: 2020-04-29
Publish Date: 2020-07-15

Abstract

Abstract

Daolundaba Cu polymetallic deposit islocated in southern segment of Great Hinggan Ling metallogenic belt. In this study, we carried out chronological studies of LA-ICP-MS zircon U-Pb ages, zircon trace element and Lu-Hf isotope for the biotite granites in Daolundaba deposit. LA-ICP-MS zircon U-Pb dating results suggested that the formation age of the biotite granites range from 282.2±4.5-287.0±3.7 Ma.Lu-Hf isotope analysis of the biotite granite showed that the biotite granites had high isotopic compositions of ¹⁷⁶Hf/¹⁷⁷Hf (mean values of 0.282 770 and 0.282 769) and low isotopic compositions of ¹⁷⁶Lu/¹⁷⁷Hf (mean values of 0.002 224 and 0.001 984), ε_Hf(t) values range from 3.05-8.58 and 2.31-7.36, with older two-stage ages (730.22-1 083.46 Ma and 812.42-1 134.56 Ma). Zircon trace element results suggest eda S-type granites characteristic with al ow Nb(< 2×10^-6)values and large negative Euanomalies. The forming mean temperatures of the biotite granite calculated by zircon Tithermometer are 770℃ and 785℃, indicated that its magmas is like lytorelate to a subducted environment, and the source region probably experienced partial melting with water nearly saturation. The Daolundaba copper polymetallic deposit was formed in the Late Permian subduction environment.
- Daolundaba Cu polymetallic deposit,
- Late Paleozoic,
- zircon U-Pb dating,
- zircon trace element,
- Lu-Hf isotope,
- Xingmeng orogenic belt,
- geochemistry

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