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Origin of Bainiuchang silver-polymetallic deposit in Yunnan,China

Chaohui Zhu, Qian Zhang, Shao Shu-xun, HE Yu-liang, Dapeng Wang

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Abstract

On the basis of the geological and geochemical characteristics of the metallic deposit and its long-term multi-staged mineralization,the authors consider that the Bainiuchang silver-polymetallic deposit is a hot-water in deposit-diplogenetic deposit.The Cambrian hot-water syngenetic sedimentary ore-forming process occurred in the early stage,while the Yanshanian granitic magma hydatogenesis in the later stage.The deposit was produced by superimposition of the hot-water sedimentary mineralization and magmatic hydatogenesis.

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What this paper is about

On the basis of the geological and geochemical characteristics of the metallic deposit and its long-term multi-staged mineralization,the authors consider that the Bainiuchang silver-polymetallic deposit is a hot-water in deposit-diplogenetic deposit.The Cambrian hot-water syngenetic sedimentary ore-forming process occurred in the early stage,while the Yanshanian granitic magma hydatogenesis in the later stage.The deposit was produced by superimposition of the hot-water sedimentary mineralization and magmatic hydatogenesis.

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Available abstract

On the basis of the geological and geochemical characteristics of the metallic deposit and its long-term multi-staged mineralization,the authors consider that the Bainiuchang silver-polymetallic deposit is a hot-water in deposit-diplogenetic deposit.The Cambrian hot-water syngenetic sedimentary ore-forming process occurred in the early stage,while the Yanshanian granitic magma hydatogenesis in the later stage.The deposit was produced by superimposition of the hot-water sedimentary mineralization and magmatic hydatogenesis.

Key concepts: Geology, Mineralization (soil science), Geochemistry, Sedimentary rock, Stage (stratigraphy), Paleontology, Soil water, Soil science

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