Abstract
The granite in this area has been dated by Rb-Sr at 99 to 115 Ma, and its genesis is discussed.
The isotope compositions of Pb, S, O, C of the minerals at various ore-forming stages of every belt in the orefield have been measured, and their variation regularities are interpreted. The genesis and source matter of the deposits are also discussed.
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© 1988 United Nations New York
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Wenkin, X., Qinsheng, W., Junzhen, X. (1988). Isotope Geochemistry of the Dachang Tin-Polymetallic Ore-Field. 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_31
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DOI: https://doi.org/10.1007/978-3-642-72765-8_31
Publisher Name: Springer, Berlin, Heidelberg
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