Geology, geochronology and geochemistry of the Gaogangshan Mo deposit: A newly discovered Permo-Triassic collision-type Mo mineralization in the Lesser Xing'an Range, NE China
Mineralized S-type granitoids are generated by anatexis of metasedimentary rocks. Ore fluids are derived from a mixture of magmatic and meteoric water. Ore materials are mainly originated from magma of orogenic belt. Timing of magmatism and Mo mineralization are Permo-Triassic. A newly discovered collision-type porphyry Mo deposit in the Lesser Xing'an Range