东昆仑祁漫塔格地区乌兰乌珠尔早古生代花岗岩锆石U-Pb年代学、地球化学及其地质意义

韩志辉; 孙丰月; 田楠; 高宏昶; 李良; 赵拓飞

doi:10.3799/dqkx.2020.067

Volume 46 Issue 1

Jan. 2021

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Han Zhihui, Sun Fengyue, Tian Nan, Gao Hongchang, Li Liang, Zhao Tuofei, 2021. Zircon U-Pb Geochronology, Geochemistry and Geological Implications of the Early Paleozoic Wulanwuzhuer Granites in the Qimantag, East Kunlun, China. Earth Science, 46(1): 13-30. doi: 10.3799/dqkx.2020.067

Citation:

Han Zhihui, Sun Fengyue, Tian Nan, Gao Hongchang, Li Liang, Zhao Tuofei, 2021. Zircon U-Pb Geochronology, Geochemistry and Geological Implications of the Early Paleozoic Wulanwuzhuer Granites in the Qimantag, East Kunlun, China. Earth Science, 46(1): 13-30. doi: 10.3799/dqkx.2020.067

Citation:

Han Zhihui, Sun Fengyue, Tian Nan, Gao Hongchang, Li Liang, Zhao Tuofei, 2021. Zircon U-Pb Geochronology, Geochemistry and Geological Implications of the Early Paleozoic Wulanwuzhuer Granites in the Qimantag, East Kunlun, China. Earth Science, 46(1): 13-30. doi: 10.3799/dqkx.2020.067

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Zircon U-Pb Geochronology, Geochemistry and Geological Implications of the Early Paleozoic Wulanwuzhuer Granites in the Qimantag, East Kunlun, China

doi: 10.3799/dqkx.2020.067

Han Zhihui^{1
,
,},
Sun Fengyue^{1
,
,
,},
Tian Nan¹,
Gao Hongchang¹,
Li Liang²,
Zhao Tuofei¹

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
School of Resource Environment and Earth Science, Yunnan University, Kunming 650000, China

Received Date: 2020-02-11
Publish Date: 2021-01-15

Abstract

Abstract

In order to determine the formation time,petrogenesis,magma source and tectonic setting of gneissic biotite granites and the monzonotic granites in the wulanwuzhuer area of Qimantag,East Kunlun.Zircon U-Pb geochronology,geochemistry and HF isotopes of the rocks have been studied.The results show that:The weighted mean age of gneissic biotite granites is 457.5±2.3 Ma,and the A/CNK is between 0.98-1.02,belonging to sub-aluminous rocks.The ratio of Na₂O/K₂O is between 0.440-0.625,which belongs to high-K calc-alkaline series.The weighted mean age of the Monzonotic granites is 422.5±1.6 Ma,and the A/CNK is between 1.03-1.05,belonging to the weakly peraluminous rocks.Both of them have the characteristics of high SiO₂ (SiO₂ between 68.93% and 74.72%),high alkali (all alkali ALK between 6.83% and 9.40%),low P₂O₅ (P₂O₅ less than 0.12%).Enrichment of LREE and depletion of HREE,and δEu is between 0.29-0.70,indicating that Eu is moderately negative.These samples are enriched in LILE (such as Rb、K) and depleted in HFSE (such as Nb、Ta、P、Ti),belongs to I-type granites.The ε_Hf(t) values of zircon from the monzonotic granites range from -2.2 to +1.4,their Hf two-stage model ages vary from 1.32 Ga to 1.54 Ga.Combined with the geochronological data,geochemical characteristics and regional tectonic evolution,the gneissic biotite granite (457.5±2.3 Ma) is a partial melting product of the lower crust,which was formed in the local tensional environment of the North subduction of the Proto-Tethys.The monzonotic granitic (422.5±1.6 Ma) magma is derived from the partial melting products of the juvenile lower crust in Mesoproterozoic.it is considered that the rocks should be formed in the post-collisional extension setting.
- granite,
- geochemistry,
- zircon U-Pb diating,
- Hf istope,
- Qimantag

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References(106)

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Zircon U-Pb Geochronology, Geochemistry and Geological Implications of the Early Paleozoic Wulanwuzhuer Granites in the Qimantag, East Kunlun, China

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