Geology, Mineralization, and Fluid Inclusion Characteristics of the Kashkasu W-Mo-Cu Skarn Deposit Associated with a High-Potassic to Shoshonitic Igneous Suite in Kyrgyzstan, Tien Shan: Toward a Diversity of W Mineralization in Central Asia

Volume: 153, Pages: 425 - 449
Published: Mar 1, 2018
Abstract
null null The Kashkasu deposit is part of the subduction-related Late Paleozoic (Late Carboniferous) metallogenic belt of Tien Shan. It is associated with a multiphase monzodiorite-monzonite-granodiorite-granite pluton of the magnetite-series high-K calc-alkaline to shoshonitic igneous suite. The deposit contains zones of W-Mo-Cu oxidized prograde and retrograde skarns, with abundant andraditic garnet, magnetite, locally scapolite and...
Paper Details
Title
Geology, Mineralization, and Fluid Inclusion Characteristics of the Kashkasu W-Mo-Cu Skarn Deposit Associated with a High-Potassic to Shoshonitic Igneous Suite in Kyrgyzstan, Tien Shan: Toward a Diversity of W Mineralization in Central Asia
Published Date
Mar 1, 2018
Volume
153
Pages
425 - 449
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