大别山皇城山银矿区及外围陈棚组火山岩U-Pb年代学、地球化学和成矿构造背景

朱江; 吴昌雄; 彭三国; 彭练红; 张闯; 刘锦明

doi:10.3799/dqkx.2018.187

Volume 43 Issue 7

Jul. 2018

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Zhu Jiang, Wu Changxiong, Peng Sanguo, Peng Lianhong, Zhang Chuang, Liu Jinming, 2018. Geochronology and Geochemistry of Volcanic Rocks from the Huangchengshan Volcanogenic Epithermal Silver Deposit, Dabie Orogen, China: Implications for Tectonic Setting. Earth Science, 43(7): 2404-2419. doi: 10.3799/dqkx.2018.187

Citation:

Zhu Jiang, Wu Changxiong, Peng Sanguo, Peng Lianhong, Zhang Chuang, Liu Jinming, 2018. Geochronology and Geochemistry of Volcanic Rocks from the Huangchengshan Volcanogenic Epithermal Silver Deposit, Dabie Orogen, China: Implications for Tectonic Setting. Earth Science, 43(7): 2404-2419. doi: 10.3799/dqkx.2018.187

Citation:

Zhu Jiang, Wu Changxiong, Peng Sanguo, Peng Lianhong, Zhang Chuang, Liu Jinming, 2018. Geochronology and Geochemistry of Volcanic Rocks from the Huangchengshan Volcanogenic Epithermal Silver Deposit, Dabie Orogen, China: Implications for Tectonic Setting. Earth Science, 43(7): 2404-2419. doi: 10.3799/dqkx.2018.187

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Geochronology and Geochemistry of Volcanic Rocks from the Huangchengshan Volcanogenic Epithermal Silver Deposit, Dabie Orogen, China: Implications for Tectonic Setting

doi: 10.3799/dqkx.2018.187

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, China
3.
Sixth Geological Brigade, Hubei Geological Bureau, Xiaogan 432000, China

Received Date: 2017-08-22
Publish Date: 2018-07-15

Abstract

Abstract

The Huangchengshan deposit is the largest high-sulfidation epithermal silver deposit in the Western Dabie orogen. Silver mineralization characterized by argentiferous quartz veins is controlled by fractures of volcanic apparatus, and is spatially associated with volcanic rocks of Chenpeng Formation. In situ zircon U-Pb dating yielded 133.4±1.5 Ma (1σ, MSWD=1.3) and 133.1±0.8 Ma (1σ, MSWD=0.59) for the tuff and rhyolite from Chenpeng Formation, respectively, indicating an Early Cretaceous volcanism. The data also suggest a syngenetic volcanogenic epithermal mineralization age of ca.133 Ma for the Huangchengshan silver deposit. Rhyolites of the Chenpeng Formation display high contents of SiO₂ (73.83% to 77.38%) and K₂O (4.65% to 9.31%), belonging to high-K calc-alkaline series. Their A/CNK ratios range from 1.09 to 1.31, exhibiting peraluminous characteristics. Rare earth elements show light rare earth elements (LREEs) enrichment and flat heavy rare earth elements (HREEs) patterns, with moderate negative Eu anomalies (δEu=0.33-0.88). They are enriched in large ion lithophile elements (LILEs), but depleted in Ba, Nb, Ta, P and Ti. These geochemical characteristics show affinity to highly fractionated granites. The rhyolites have high I_Sr values (0.708 220 to 0.708 741) and negative ε_Nd(t) values (-17.2 to -18.5), with two-stage Nd model ages of 2.32 to 2.43 Ga. Zircon ε_Hf(t) values are negative (-22.3 to -26.1) with an calculated two-stage Hf model ages of 2.29 to 2.49 Ga. The geochemical and Sr-Nd-Hf isotopic signatures suggest that the rhyolite is likely to be derived by partial melting of the ancient lower crust of the Yangtze Block. We propose that this volcanism and related Huangchengshan silver deposit formed in a transitional stage from crustal compression to extension driven by delamination of thickened lower crust during the Early Cretaceous.
- silver deposits,
- volcanic rocks,
- geochronology,
- geochemistry,
- Sr-Nd-Hf isotopes,
- Dabie orogen

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References(92)

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Geochronology and Geochemistry of Volcanic Rocks from the Huangchengshan Volcanogenic Epithermal Silver Deposit, Dabie Orogen, China: Implications for Tectonic Setting

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