浙西大铜坑斑岩型钨钼矿床成岩成矿年代学

胡开明; 唐增才; 孟祥随; 周汉文; 董学发; 杜雄; 陈忠大

doi:10.3799/dqkx.2016.502

Volume 41 Issue 9

Sep. 2016

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Article Navigation > Earth Science > 2016 > 41(9): 1435-1450

Hu Kaiming, Tang Zengca, Meng Xiangsui, Zhou Hanwen, Dong Xuefa, Du Xiong, Chen Zhongda, 2016. Chronology of Petrogenesis and Mineralization of Datongkeng Porphyry W-Mo Deposit in West Zhejiang. Earth Science, 41(9): 1435-1450. doi: 10.3799/dqkx.2016.502

Citation:

Hu Kaiming, Tang Zengca, Meng Xiangsui, Zhou Hanwen, Dong Xuefa, Du Xiong, Chen Zhongda, 2016. Chronology of Petrogenesis and Mineralization of Datongkeng Porphyry W-Mo Deposit in West Zhejiang. Earth Science, 41(9): 1435-1450. doi: 10.3799/dqkx.2016.502

Citation:

Hu Kaiming, Tang Zengca, Meng Xiangsui, Zhou Hanwen, Dong Xuefa, Du Xiong, Chen Zhongda, 2016. Chronology of Petrogenesis and Mineralization of Datongkeng Porphyry W-Mo Deposit in West Zhejiang. Earth Science, 41(9): 1435-1450. doi: 10.3799/dqkx.2016.502

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Chronology of Petrogenesis and Mineralization of Datongkeng Porphyry W-Mo Deposit in West Zhejiang

doi: 10.3799/dqkx.2016.502

1.
Zhejiang Institute of Geological Survey, Hangzhou 311203, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
4.
No.1 Geological Party of Zhejiang Province, Hangzhou 311200, China

Received Date: 2016-01-11
Publish Date: 2016-09-15

Abstract

Abstract

As an important component to reveal the metallogenic regularity in the Zhejiang-Anhui-Jiangxi border region, the Datongkeng porphyry W-Mo deposit in Chun'an County is located in the southeastern margin of the Yangtze block, and the W-Mo ore bodies are mainly located in the internal or external contact zones between granite and sandstone of Xiuning Formation. The Datongkeng granite is characterized by quasi-aluminous, showing the nature of Ⅰ-type granite and high-K calc-alkalic series rock. The granite is rich in Rb, K, Th, U, and relatively depleted in Sr, Ba, Nb, Ta, Ti. The total REE contents are relatively low (ΣREE=106.2×10^-6-211.5×10^-6), and the rocks show obvious LREE and HREE fractionation (ΣLREE/ΣHREE=6.4-12.2), moderately negative Eu anomalies (δEu=0.50-0.63), suggesting that these rocks have the characters of typical volcanic arc rocks. The SHRIMP U-Pb zircon age of 148.3±1.9 Ma for granite is close to the Re-Os isochron age of 146.47±0.81 Ma for five molybdenite samples from the Datongkeng W-Mo deposit, indicating magmatism and mineralization are a continuous process, which took place in the compression tectonic environment related to the subduction of pacific plate at Late Jurassic, and corresponds to the second large-scale W-Mo mineralization in South China.
- SHRIMP U-Pb dating of zircon,
- Re-Os age of molybdenite,
- geochemistry,
- chronology,
- Datongkeng W-Mo deposit,
- granite,
- West Zhejiang

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References(109)

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Chronology of Petrogenesis and Mineralization of Datongkeng Porphyry W-Mo Deposit in West Zhejiang

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