Geology, Mineralization, and Fluid Inclusion Characteristics of the Kensu W-Mo Skarn and Mo-W-Cu-Au Alkalic Porphyry Deposit, Tien Shan, Kyrgyzstan

The Kensu deposit is located within a large metallogenic belt of W-Mo, Cu-Mo, W-Au, Au, and Pb-Zn deposits along the Late Paleozoic active continental margin of Tien Shan. The deposit is related to a small Late Carboniferous to Early Permian multiphase gabbro-monzonite(syenite)-granite pluton representing an alkaline potassic (shoshonitic) suite. The igneous rocks are related to a deep-rooted magmatic source but the pluton emplacement...