东秦岭东段五垛山花岗伟晶岩锆石U-Pb年代学和微量元素特征及地质意义

陈孝珍; 陈国超; 李瑞保; 张亚峰; 季宪军; 张晓飞

doi:10.3799/dqkx.2021.206

Volume 48 Issue 10

Oct. 2023

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Chen Xiaozhen, Chen Guochao, Li Ruibao, Zhang Yafeng, Ji Xianjun, Zhang Xiaofei, 2023. Zircon U-Pb Geochronology and Trace Element Characteristics of Wuduoshan Granitic Pegmatite in Eastern Part of East Qinling and Its Geological Significance. Earth Science, 48(10): 3753-3769. doi: 10.3799/dqkx.2021.206

Citation:

Chen Xiaozhen, Chen Guochao, Li Ruibao, Zhang Yafeng, Ji Xianjun, Zhang Xiaofei, 2023. Zircon U-Pb Geochronology and Trace Element Characteristics of Wuduoshan Granitic Pegmatite in Eastern Part of East Qinling and Its Geological Significance. Earth Science, 48(10): 3753-3769. doi: 10.3799/dqkx.2021.206

Citation:

Chen Xiaozhen, Chen Guochao, Li Ruibao, Zhang Yafeng, Ji Xianjun, Zhang Xiaofei, 2023. Zircon U-Pb Geochronology and Trace Element Characteristics of Wuduoshan Granitic Pegmatite in Eastern Part of East Qinling and Its Geological Significance. Earth Science, 48(10): 3753-3769. doi: 10.3799/dqkx.2021.206

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Zircon U-Pb Geochronology and Trace Element Characteristics of Wuduoshan Granitic Pegmatite in Eastern Part of East Qinling and Its Geological Significance

doi: 10.3799/dqkx.2021.206

Chen Xiaozhen^{1, 2
,
,},
Chen Guochao^{2, 3
,
,
,},
Li Ruibao²,
Zhang Yafeng⁴,
Ji Xianjun¹,
Zhang Xiaofei⁵

1.
School of Civil Engineering, Nanyang Institute of Technology, Nanyang 473000, China
2.
Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, China
3.
Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources, Beijing 100037, China
4.
Shaanxi Center of Mineral Geological Survey, Xi'an 710068, China
5.
Development Research Center, China Geological Survey, Beijing 100037, China

Received Date: 2021-08-21
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

The granitic pegmatite exposed in Wuduoshan granitic pluton occurs extensively in volume. However, its formation time, petrogenesis and geodynamic background are still unclear. LA-ICP-MS zircon U-Pb dating shows that the zircon U-Pb ages from the granitic pegmatite are 417.4±2.5, 429.5±2.1 and 450.9±3.3 Ma, respectively, the first of which represents the crystallization age of granitic pegmatite and the other is consistent with the age of Wuduoshan granite batholith, representing the captured zircons from the surrounding rocks of granitic pegmatite veins. The ε_Hf(t) values of granitic pegmatite are -5.6 to -1.9, -8.7 to -1.3, and -5.3 to -3.4, respectively, which are similar to the Hf isotopic values of magmatic rocks derived from partial melting of metasedimentary rocks of the Qinling Group. Together with the regional data, it is suggested that the East Qinling was in the post-collision stage relevant to the proto-Tethys Ocean in the Early Devonian, and it underwent extensional setting and resulting the decompression melting of mantle and generation of mafic magma. The rising high-temperature magma further underplated and heated the lower crust and induced the partial melting of metamorphic basement of the lower crust, ultimately generating the granitic pegmatites along the magmatic conduits which formed in a postcollision-related extensional setting.
- East Qinling,
- granitic pegmatite,
- zircon LA-ICP-MS dating,
- trace elements,
- petrology

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References(127)

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