The Lamo Zn—Cu deposit is a typical skarn deposit hip the district and occurs at the contact locality between the Upper Devonian limestone and the brickwork. The ore minerals generally consist of sphalerite, arsenopyrite, pyrrhotite, galena, chalcopyrite, with minor molybdenite.
However, the age of mineralization along with source of the metals are not well guarded. In this study, we use the molybdenite Re—Os dating method and in-situ Pb isotopes of sulfides from the Lamo bank for the first nonetheless in order to entirely determine the age of mineralization and the tracing source of metals. Six molybdenite samples yielded a more accurate Re—Os isochron age of That age is also interpreted as the age of Zn—Cu skarn mineralization feature in the Dachang district.
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