相山铀矿田邹家山矿床英安斑岩脉锆石U-Pb年代学、地球化学、Hf同位素组成及其地质意义

王勇剑; 林锦荣; 胡志华; 东前; 刘瑞萍; 庞雅庆; 高飞; 陶意

doi:10.3799/dqkx.2019.257

Volume 46 Issue 1

Jan. 2021

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Article Navigation > Earth Science > 2021 > 46(1): 31-42

Wang Yongjian, Lin Jinrong, Hu Zhihua, Dong Qian, Liu Ruiping, Pang Yaqing, Gao Fei, Tao Yi, 2021. Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Compositions of Dacitic Porphyry in Zoujiashan Deposit of Xiangshan Uranium Orefield and Its Geological Implication. Earth Science, 46(1): 31-42. doi: 10.3799/dqkx.2019.257

Citation:

Wang Yongjian, Lin Jinrong, Hu Zhihua, Dong Qian, Liu Ruiping, Pang Yaqing, Gao Fei, Tao Yi, 2021. Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Compositions of Dacitic Porphyry in Zoujiashan Deposit of Xiangshan Uranium Orefield and Its Geological Implication. Earth Science, 46(1): 31-42. doi: 10.3799/dqkx.2019.257

Citation:

Wang Yongjian, Lin Jinrong, Hu Zhihua, Dong Qian, Liu Ruiping, Pang Yaqing, Gao Fei, Tao Yi, 2021. Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Compositions of Dacitic Porphyry in Zoujiashan Deposit of Xiangshan Uranium Orefield and Its Geological Implication. Earth Science, 46(1): 31-42. doi: 10.3799/dqkx.2019.257

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Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Compositions of Dacitic Porphyry in Zoujiashan Deposit of Xiangshan Uranium Orefield and Its Geological Implication

doi: 10.3799/dqkx.2019.257

Beijing Research Institute of Uranium Geology, Beijing 100029, China

Received Date: 2019-10-16
Publish Date: 2021-01-15

Abstract

Abstract

Geochemistry,zircon U-Pb geochronology and Hf isotopic compositions of dacitic porphyry discovered in the Zoujiashan deposit were studied for the first time in Xiangshan uranium deposit. The LA-ICP-MS zircon U-Pb age testing results show that the average weighted age of two samples collected from underground tunnel and open pit were 122.4±0.5 Ma and 126.5±1.4 Ma,respectively,which were formed much later than the large-scale volcanic-intrusive activity. The rock is characterized by negative Eu anomalies,light-heavy REE fractionation,enrichment of large lithophilic elements as well as negative anomalies in Nb and Ta. The zircon ε_Hf(t) values range from -22.0 to 0.2,most of which are concentrated between -6 and -10,and the two-stage Hf model age t_DM2 range from 1 170 to 2 575 Ma,which share the similar characteristics with the Xiangshan volcanic rocks and subvolcanic rocks. The trace element and zircon Hf isotopic analysis showed that the dacitic porphyry was mainly derived from partial melting of crust material,but the participation of mantle material could not be ruled out. In combination with previous data,it is believed that the dacitic porphyry and the intermediate-basic dikes were probably formed in the lithospheric extension environment caused by the continuous retreat of the Pacific subduction plate during the Early-Middle Cretaceous period,and were the typical products of the lithospheric thinning in South China.
- dacitic porphyry,
- LA-ICP-MS zircon U-Pb age,
- Hf isotope,
- Zoujiashan deposit,
- Xiangshan orefield,
- geochemistry,

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Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Compositions of Dacitic Porphyry in Zoujiashan Deposit of Xiangshan Uranium Orefield and Its Geological Implication

doi: 10.3799/dqkx.2019.257

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通讯作者: 陈斌, bchen63@163.com

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