Abstract
AbstractTheDaheishanMo deposit is located in the eastern part of theCentralAsianOrogenicBelt,NE China. Rhenium and osmium isotopes of molybdenites from theDaheishan deposit were used to determine the age of mineralization. Rhenium concentrations in molybdenite samples are between 17 and 30μg g−1. Analysis of seven molybdenite samples yields an isochron age of 168.0 ± 4.4 Ma (2σ). Based on the geological history and spatial‐temporal distribution of the granitoids, it is proposed that theMo deposits in easternChina were related to the subduction of the Paleo‐Pacific plate during Jurassic time.
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