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A New Type of Tin Deposit — The Yinyan Porphyry Tin Deposit in China

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Abstract

The Yinyan tin-bearing granites are composite. They yield a K-Ar age of about 92 Ma, therefore they appear to be late Yenshanian. They are oversatured, peralkaline and rich in fluorine, tin, molybdenum and bismuth. They have a REE pattern which is similar to the S-type granites of south China. Explosive volcanic phenomena can generally be seen at the top of granites.

Orebodies occur at the upper part of these granites, which have the shape of an inverted cup. Ore minerals are mainly major cassiterite and subordinate wolframite, bismuthinite and molybdenite. Ores are characterized by a hypidiomorphic texture and veinlet-impregnation structure. Four alteration zones can be recognized: (1) chlorite hornfels zone; (2) topaz-greisen zone, which forms the main portion of mineralization; (3) the incorporated potassium-silicate zone; and (4) the potash-silicate zone. Fluid inclusion study has demonstrated that the temperature at the time of mineralization varied from 160 to 360° C.

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References

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© 1988 United Nations New York

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Xunfan, G., Yongqin, S., Jinghua, X., Shuzhao, L., Jinmao, L. (1988). A New Type of Tin Deposit — The Yinyan Porphyry Tin Deposit in China. In: Hutchison, C.S. (eds) Geology of Tin Deposits in Asia and the Pacific. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-72765-8_38

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  • DOI: https://doi.org/10.1007/978-3-642-72765-8_38

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-72767-2

  • Online ISBN: 978-3-642-72765-8

  • eBook Packages: Springer Book Archive

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