Rock-Forming and Ore-Forming Ages of the Baizhangyan Tungsten-Molybdenum
Baizhangyan tungsten-molybdenum ore deposit is a newly developed deposit which was found on the base of a small exposure of mineralization occurrence. With highly precise dating of the ages of the rock-forming and ore-forming, the authors obtained a SHRIMP U-Pb zircon age of (130±1.5) Ma (n=14, MSWD=0.69) for fine-grained granite and Re-Os model ages of (133.5±1.9)-(135.6±2.0) Ma and isochron age of (136.3±2.6) Ma (n=5, MSWD=0.64). According to the ages above, the authors concluded that the deposit was formed in the Early Cretaceous; that it was the result of intrusions of the granite which was of crustsource remelting type. The ore-forming age is similar to the rock-forming age of the granite rock body that was important to the deposit.
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