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The Qinling Molybdenum Belt

More than 90% of the molybdenum reserves so far discovered in the Qinling molybdenum belt are associated with the Palaeozoic Erlangping back-arc basin.

Compiled Re-Os isotopic ages for porphyry deposits (including several carbonate vein deposits) that have been dated show peaks during 220 million years (>0.32 Mt), 145 million years (>3.5 Mt), and 115 million years (>0.84 Mt).

Which correlate well with the three major episodes of granitoid magmatism since the Triassic.
 

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