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Consequently, genetic models for ore formation are poorly constrained and remain controversial.

The deposit has a grade of 0.06% Mo and a high content of rhenium of 1.4 g/t.Analysis of eight molybdenite samples yields an isochron age of 224.8±4.5 Ma (2σ).Pyrite samples have rhenium and osmium concentrations varying in the range 33.4–330.6 ng/g and 0.08–0.81 ng/g, respectively.Rhenium and osmium isotopes in sulfide minerals from the Baishan deposit are used to determine the age of mineralization.Rhenium concentrations in molybdenite samples are between 74 and 250 μg/g.

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