Highly Oxidized Magma and Fluid Evolution of Miocene Qulong Giant Porphyry Cu-Mo Deposit, Southern Tibet, China

Porphyry Copper Systems

(2010) R. H. Sillitoe   ECONOMIC GEOLOGY

Sulfur content at sulfide saturation in oxidized magmas

(2009) Pedro J. Jugo   GEOLOGY

Apatite Composition: Tracing Petrogenetic Processes in Transhimalayan Granitoids

(2009) Mei-Fei Chu et al.   JOURNAL OF PETROLOGY

Geology of the post-collisional porphyry copper–molybdenum deposit at Qulong, Tibet

(2009) Zhiming Yang et al.   ORE GEOLOGY REVIEWS

Contribution of syncollisional felsic magmatism to continental crust growth: A case study of the Paleogene Linzizong volcanic Succession in southern Tibet

(2008) Xuanxue Mo et al.   CHEMICAL GEOLOGY

Synthetic Fluid Inclusions. XVII. PVTX Properties of High Salinity H2O-NaCl Solutions (>30 wt % NaCl): Application to Fluid Inclusions that Homogenize by Halite Disappearance from Porphyry Copper and Other Hydrothermal Ore Deposits

(2008) S. P. Becker et al.   ECONOMIC GEOLOGY

Anhydrite-bearing andesite and dacite as a source for sulfur in magmatic-hydrothermal mineral deposits

(2008) Isabelle Chambefort et al.   GEOLOGY

Primary igneous anhydrite: Progress since its recognition in the 1982 El Chichón trachyandesite

(2008) James F. Luhr   JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH

The Miocene Gangdese porphyry copper belt generated during post-collisional extension in the Tibetan Orogen

(2008) Zengqian Hou et al.   ORE GEOLOGY REVIEWS

The origin of S4+ detected in silicate glasses by XANES

(2007) M. Wilke et al.   AMERICAN MINERALOGIST