The pre- and syn-ore granites developed at Late Carboniferous to Early Permian.
Molybdenite Re-Os dating show different mineralization ages at various deposits.
The granites contain unfractionated and fractionated calc-alkaline I-type rocks.
Sr-Nd-Pb-Hf-O isotopes indicate crustal assimilation was important.
The granites are formed during subduction and syn-collision stages.
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