辽东地区中生代花岗岩的侵位时代：锆石和独居石U-Pb年代学

胡国辉; 张琪琪; 李建锋; 张拴宏

doi:10.3799/dqkx.2020.293

Volume 45 Issue 11

Nov. 2020

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Article Navigation > Earth Science > 2020 > 45(11): 3962-3981

Hu Guohui, Zhang Qiqi, Li Jianfeng, Zhang Shuanhong, 2020. Emplacement Ages of Mesozoic Granites in Liaodong Area: Constraints from Zircon and Monazite U-Pb Dating. Earth Science, 45(11): 3962-3981. doi: 10.3799/dqkx.2020.293

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Hu Guohui, Zhang Qiqi, Li Jianfeng, Zhang Shuanhong, 2020. Emplacement Ages of Mesozoic Granites in Liaodong Area: Constraints from Zircon and Monazite U-Pb Dating. Earth Science, 45(11): 3962-3981. doi: 10.3799/dqkx.2020.293

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Emplacement Ages of Mesozoic Granites in Liaodong Area: Constraints from Zircon and Monazite U-Pb Dating

doi: 10.3799/dqkx.2020.293

Hu Guohui^{1, 2
,
,},
Zhang Qiqi¹,
Li Jianfeng^{1, 2},
Zhang Shuanhong^{1, 2}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China

Received Date: 2020-05-31
Publish Date: 2020-11-15

Abstract

Abstract

The Mesozoic magmatic activities extensively developed in East Liaoning Province accompanied by large-scale gold mineralization. Wulong gold deposit is a representative largest quartz-vein type gold deposit,and the gold ore bodies mainly hosted in Jurassic gneiss biotite granite and Early Cretaceous granodiorite. Therefore,Mesozoic magmatism has a significant genetic relation with the gold mineralization. In this paper,it presents zircon and monazite U-Pb dating of gneiss granite and Sanguliu rock mass in Wulong gold ore-concentrated district to constrain their emplacement ages. The gneiss granite is dominated by biotite monzogranite,the minerals of which show strong ductile deformation and are oriented. Their zircon U-Pb ages are 159.2±1.8 Ma,160.2±1.8 Ma,and 156.1±1.2 Ma,respectively. Zircons from Sanguliu biotite monzogranite yield a U-Pb age of 123.8±1.2 Ma. Mineralogical characteristics and chemical compositions of monazites from four granitic samples suggest a magmatic origin. New LA-ICP-MS dating of monazites from three gneiss granite samples yielded U-Pb ages of 158.1±1.9 Ma,157.5±1.4 Ma,and 153.5±1.4 Ma,respectively,and 123.4±1.5 Ma for Sanguliu biotite monzogranite. Monazite ages of Late Jurassic gneiss granite are 1.1-2.7 Ma younger than their zircon ages,two of which have high cooling rate of 55.56℃/Ma and 57.69℃/Ma,suggesting a rapid cooling process and crustal uplift. Both zircon and monazite U-Pb ages indicate that the gneiss granite and Sanguliu rock mass formed during Late Jurassic and Early Cretaceous,respectively. In combination with the available data,Wulong gold ore-concentrated district mainly developed Late Jurassic and Early Cretaceous magmatic activities,which were closely related to the subduction of Paleo-Pacific plate to Eurasia continent,accompanied by Early Cretaceous gold mineralization.
- East Liaoning Province,
- Mesozoic granite,
- zircon and monazite U-Pb dating,
- gold deposit,
- geochronology

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References(89)

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Emplacement Ages of Mesozoic Granites in Liaodong Area: Constraints from Zircon and Monazite U-Pb Dating

doi: 10.3799/dqkx.2020.293

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