| Qinling-Type Lead-Zinc Deposits |
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| 作者单位： | Li Jianzhong，Gansu Institute of Geology for Non-Ferrous Metals，CNNC，Lanzhou，Gansu He Dianren North west Institute of Geology for Non-Ferrous Metals，CNNC，Xi'an，Shaanxi and Wu Jianmin Research Institute of Geology for Mineral Resources，CNNC，Guilin，Guangxi |
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| 摘 要： | Qinling-type Pb-Zn deposits are located in the Qinling fold belt, occurring in the fine-clastic and carbonate rocks of the Devonian marine facies. They are reformed sedimentary deposits originating from hydrothermal waters, and may be subdivided into 2 subtypes: hydrothermal sedimentary deposits (Changba subtype) and reformed hydrothermal sedimentary deposits (Bijiashan-Qiandongshan subtype). In comparison with some of the famous Palaeozoic Pb-Zn deposits in the world, the Qinling-type Pb-Zn deposits constitute an independent type, which possesses some characteristics of both hydrothermal sedimentary deposits (Meggen type) and reformed hydrothermal deposits (Mississippi Valley type).
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Qinling-Type Lead-Zinc Deposits |
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| Li Jianzhong,Gansu Institute of Geology for Non-Ferrous Metals,CNNC,Lanzhou,Gansu He Dianren North west Institute of Geology for Non-Ferrous Metals,CNNC,Xi''an,Shaanxi and Wu Jianmin Research Institute of Geology for Mineral Resources,CNNC,Guilin,Guangxi. Qinling-Type Lead-Zinc Deposits[J]. Acta Geologica Sinica (English Edition), 1993, 67(1) |
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| Authors: | Li Jianzhong Gansu Institute of Geology for Non-Ferrous Metals CNNC Lanzhou Gansu He Dianren North west Institute of Geology for Non-Ferrous Metals CNNC Xi''an Shaanxi Wu Jianmin Research Institute of Geology for Mineral Resources CNNC Guilin Guangxi |
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| Abstract: | Qinling-type Pb-Zn deposits are located in the Qinling fold belt, occurring in the fine-clastic and carbonate rocks of the Devonian marine facies. They are reformed sedimentary deposits originating from hydrothermal waters, and may be subdivided into 2 subtypes: hydrothermal sedimentary deposits (Changba subtype) and reformed hydrothermal sedimentary deposits (Bijiashan-Qiandongshan subtype). In comparison with some of the famous Palaeozoic Pb-Zn deposits in the world, the Qinling-type Pb-Zn deposits constitute an independent type, which possesses some characteristics of both hydrothermal sedimentary deposits (Meggen type) and reformed hydrothermal deposits (Mississippi Valley type). |
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| Keywords: | Qinling-type lead zinc deposit Changba subtype. Bijiashan-Qiandongshan subtype |
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