大兴安岭中段塔尔气地区中酸性火山岩成因及构造背景

陈超; 吕新彪; 李杰; 衮民汕

doi:10.3799/dqkx.2020.317

Volume 45 Issue 12

Dec. 2020

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Article Navigation > Earth Science > 2020 > 45(12): 4446-4462

Chen Chao, Lü Xinbiao, Li Jie, Gun Minshan, 2020. Petrogenesis and Tectonic Setting of Intermediate-Felsic Volcanics in Ta'erqi Area, Central Great Xing'an Range. Earth Science, 45(12): 4446-4462. doi: 10.3799/dqkx.2020.317

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Chen Chao, Lü Xinbiao, Li Jie, Gun Minshan, 2020. Petrogenesis and Tectonic Setting of Intermediate-Felsic Volcanics in Ta'erqi Area, Central Great Xing'an Range. Earth Science, 45(12): 4446-4462. doi: 10.3799/dqkx.2020.317

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Petrogenesis and Tectonic Setting of Intermediate-Felsic Volcanics in Ta'erqi Area, Central Great Xing'an Range

doi: 10.3799/dqkx.2020.317

Chen Chao^{1
,
,},
Lü Xinbiao^{1
,
,
,},
Li Jie²,
Gun Minshan³

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
No. 230 Institute of Nuclear Industry, Changsha 410007, China
3.
Non-Ferrous Matals and Nuclear Industry Geological Exploration Bureau of Guizhou, Guiyang 550005, China

Received Date: 2020-07-14
Publish Date: 2020-12-15

Abstract

Abstract

In order to study the petrogenesis and tectonic setting of intermediate-felsic volcanics in Ta'erqi area, central Great Xing'an Range and promote the comparative study of Mesozoic volcanics in this region, in this paper it presents a synthesis study of zircon U-Pb chronology, geochemistry and Hf isotopes of volcanics from Manketouebo and Baiyingaolao formations. Zircon U-Pb dating yielded weighted mean ages of 154±2 Ma and 154±3 Ma of Manketouebo Formation and 132±2 Ma of Baiyingaolao Formation.The samples are weak peraluminous with high alkali, low Mg and Ca contents, while existing the enrichment of Rb, K, Zr, Hf and depletion of Eu, Sr, Ba, P, Ti with moderate to strong negative Eu anomalies. The average zirconium saturation temperature are 915 ℃ and 841 ℃, respectively, showing the characteristics of A-type rhyolite. The ε_Hf(t) values range from +6.9 to +8.4 and +6.7 to +7.9, while the t_DM2 values range from 624 Ma to 670 Ma and 611 Ma to 682 Ma, indicating that the magma originated from the the partial melting of Neoproterozoic young crust accreted from the depleted mantle. Manketouebo Formation in Ta'erqi area formed in the early stage of extensional tectonic setting after the closure of Mongolia-Okhotsk ocean, while Baiyingaolao Formation was caused by the lithosphere extension and delamination after the closure of the Mongolia-Okhotsk Ocean and the back-arc extension induced by the subduction of the paleo-Pacific plate to Eurasia.
- central Great Xing'an Range,
- zircon U-Pb dating,
- Hf isotope,
- A-type rhyolites,
- lithosphere extension,
- deposits

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References(73)

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