Abstract
Geochemical constraints on the thermal brine genesis of the Wulagen Pb-Zn deposit in Xinjiang, have been investigated by examining fluid inclusions, physicochemical conditions such as temperature, pressure, alkalinity-acidity, salinity, REE compositions, an Pb isotopes. A comparative study was also carried out between the Wulagen and Jinding deposits in terms of REE patterns, Pb and S isotopes,and model ages of Pb isotopes (Doe, 1974). This study lends support to the thermal brine genesis of the Wulagen deposit.
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CITATION STYLE
Gao, Z., Fang, W., Hu, R., & Liu, J. (2005). Geochemical constraints on thermal brine genesis of Wulagen Pb-Zn deposit, Wuqia, Xinjiang, China. In Mineral Deposit Research: Meeting the Global Challenge (pp. 957–960). Springer Berlin Heidelberg. https://doi.org/10.1007/3-540-27946-6_244
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