西藏拉抗俄斑岩Cu-Mo矿床含矿斑岩地球化学、锆石U-Pb年代学及Hf同位素组成

冷秋锋; 唐菊兴; 郑文宝; 王保宏; 唐攀; 王豪

doi:10.3799/dqkx.2016.083

Volume 41 Issue 6

Jun. 2016

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Leng Qiufeng, Tang Juxing, Zheng Wenbao, Wang Baohong, Tang Pan, Wang Hao, 2016. Geochronology, Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakang'e Porphyry Cu-Mo Deposit, Tibet. Earth Science, 41(6): 999-1015. doi: 10.3799/dqkx.2016.083

Citation:

Leng Qiufeng, Tang Juxing, Zheng Wenbao, Wang Baohong, Tang Pan, Wang Hao, 2016. Geochronology, Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakang'e Porphyry Cu-Mo Deposit, Tibet. Earth Science, 41(6): 999-1015. doi: 10.3799/dqkx.2016.083

Citation:

Leng Qiufeng, Tang Juxing, Zheng Wenbao, Wang Baohong, Tang Pan, Wang Hao, 2016. Geochronology, Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakang'e Porphyry Cu-Mo Deposit, Tibet. Earth Science, 41(6): 999-1015. doi: 10.3799/dqkx.2016.083

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Geochronology, Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakang'e Porphyry Cu-Mo Deposit, Tibet

doi: 10.3799/dqkx.2016.083

1.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
2.
MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
4.
Institute of Geological Survey and Mineral Exploration, Inner Mongolia, Hohhot 010010, China

Received Date: 2015-11-30
Publish Date: 2016-06-15

Abstract

Abstract

The Lakang'e Cu-Mo deposit is a typical porphyry deposit in the eastern Gangdese metallogenic belt, on which previous geochemical studies are not adequate and systematic.In this paper, we present the results of the systematic logging of drillholes and provide new petrological zircon U-Pb age, and Hf isotope data for the deposit that allow the identification of the timing of formation and mineralization of the Lakang'e porphyry Cu-Mo deposit and the relationship between this deposit and other porphyry-type deposits in the Gangdese belt.Chemical analyses show that the ore-bearing granodiorite-porphyry has high SiO₂, low Mg and Ca (SiO₂=62.51% to 72.41%, MgO=0.59% to 1.30%, CaO=0.95% to 3.44%), highalkaline (Na₂O=3.51% to 4.75%, K₂O=3.30% to 4.97%), metaluminous (A/CNK=0.90 to 1.01), enriched in LILES such as Rb, Ba, Th, U, Sr, and depleted in HFSES such as Nb, Ta, Ti, P and Zr. The rocks also display low total REEcontents (∑REE=82.80×10^-6 to 132.09×10^-6), enriched LREE and differentiate obviously, with weakly negative Eu and Ce anomalies. LA-ICP-MS zircon U-Pb dating indicates that the Lakang'e ore-bearing granodiorite-porphyry emplaced at 13.58±0.42 Ma. ε_Hf(t) values and two-stage model ages of zircons are -3.99 to 4.49 and 808 to 1349 Ma respectively. The results indicate that the ore-bearing granodiorite-porphyry in the Lakang'e deposit has adakitegeochemical characteristics, and the parental magmas were mainly derived from a juvenile crust and partly mixed with old continental crust rock during the evolution. The porphyry in Lakang'edeposit was formed in post-collisional extension setting of India-Asia continental collision orogenic belt.
- geochemistry,
- zircon U-Pb dating,
- Hf isotopic compositions,
- Gangdese metallogenic belt,
- Tibet

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References(135)

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Geochronology, Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakang'e Porphyry Cu-Mo Deposit, Tibet

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