Magmatic and Tectonic Controls on the Development of Cenozoic Porphyry Cu-Mo±Au Deposits in the Gangdese Belt, Southern Tibet.

The article reports on role of collisional tectonism, magmatism, and post-subduction porphyry deposits on origin of Cenozoic Porphyry copper deposits present in Gangdese belt, Tibet, China. Topics discussed include petrographic and mineralogic analysis of Paleocene?Eocene magma rocks, overview by research scientist, E. A. Wang and colleagues, on Oligo-Miocene rocks by petrography, magmatic geochemistry, and porphyry-type mineralization and base of Cenozoic evolution by tectonomagnetism.