文摘
Dabie Shan, China is a new Mo metallogenic belt with total reserve of > 3 Mt Mo Mineralization occurred in syn- to post-collision tectonic setting during 156–110 Ma Ores associate with high-K calc-alkaline granites sourced from continental crust A scissor-style A-type subduction model is proposed for the Dabie-Qinling area The Dabie porphyry Mo belt is of collision-type, instead of rift- or subduction-type