中甸弧阿热岩体锆石U-Pb年龄、地球化学特征及岩石成因

周放; 王保弟; 刘函; 闫国川; 李小波

doi:10.3799/dqkx.2018.126

Volume 43 Issue 8

Aug. 2018

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Article Navigation > Earth Science > 2018 > 43(8): 2614-2627

Zhou Fang, Wang Baodi, Liu Han, Yan Guochuan, Li Xiaobo, 2018. Zircon U-Pb Dating, Geochemistry and Petrogenesis of Intrusive Rocks from A're Area, Zhongdian Arc. Earth Science, 43(8): 2614-2627. doi: 10.3799/dqkx.2018.126

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Zhou Fang, Wang Baodi, Liu Han, Yan Guochuan, Li Xiaobo, 2018. Zircon U-Pb Dating, Geochemistry and Petrogenesis of Intrusive Rocks from A're Area, Zhongdian Arc. Earth Science, 43(8): 2614-2627. doi: 10.3799/dqkx.2018.126

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Zircon U-Pb Dating, Geochemistry and Petrogenesis of Intrusive Rocks from A're Area, Zhongdian Arc

doi: 10.3799/dqkx.2018.126

Zhou Fang^{1,2
,},
Wang Baodi^{3
,
,},
Liu Han³,
Yan Guochuan^1,2,
Li Xiaobo³

1.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
3.
Chengdu Center of China Geological Survey, Chengdu 610081, China

Received Date: 2018-05-30
Publish Date: 2018-08-15

Abstract

Abstract

Zhongdian arc, located in Sanjiang Tethyan Orogenic belt in Southwest China southern part of Tethys belt, is one of the most important districts for polymetallic ore deposits.Previous studies mainly focus on the ore-bearing intrusions in the central and northern part of Zhongdian arc, however, there are still limited knowledge about the barren intrusions in the southern part.In this paper, we present detailed petrology, major and trace elemental geochemistry and geochronology of A're granitoids, southern part of Zhongdian arc.Zircon U-Pb dating results show the timing of emplacement of A're intrusion (216.3±1.8 Ma) is comparable to those of the other intrusive rocks in Zhongdian arc.A're quartz monzonites have high Sr (mean 1810.24×10^-6), low Y (mean 19.05×10^-6) concentrations and thus high Sr/Y(86.0-120.5) ratios.In addition, they also display enrichment in LILE (Rb, Ba, Th, U), depletion in HFSE (Nb, Ta, Ti) and slightly Eu negative anomaly, which suggests that they have geochemical characteristics of both arc-related and adakitic affinities.The low MgO (1.97%-3.30%), Ni (10.7×10^-6-26.8×10^-6), Cr (18.0×10^-6-75.8×10^-6) and Co (12.4×10^-6-17.4×10^-6) contents of the A're granitoids support that they were, generated from partial melting of thicken lower crust.Therefore, the A're quartz monzonites belong to a part of the continental marginal arc during westward subduction of Ganzi-Litang ocean, which represents the products of transformation from widespread Tethys ocean to residual sea in Zhongdian arc.
- Zhongdian arc,
- A're intrusive rocks,
- adakitic rocks,
- continental arc,
- Ganzi-Litang ocean,
- geochemistry,
- geochronology

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References(82)

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Zircon U-Pb Dating, Geochemistry and Petrogenesis of Intrusive Rocks from A're Area, Zhongdian Arc

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