Geology, mineralization, and fluid inclusion characteristics of the Kumbel oxidized W–Cu–Mo skarn and Au–W stockwork deposit in Kyrgyzstan, Tien Shan

Volume: 50, Issue: 2, Pages: 187 - 220
Published: Feb 1, 2015
Abstract
The Kumbel deposit is located within a metallogenic belt of W–Mo, Cu–Mo, Au–W, and Au deposits along the Late Paleozoic active continental margin of Tien Shan. The deposit is related to a Late Carboniferous multiphase pluton, with successive intrusive phases from early olivine monzogabbro through monzonite–quartz monzonite to granodiorite and granite, with the latest monzogabbro–porphyry dikes. The deposit represents an example of a complex...
Paper Details
Title
Geology, mineralization, and fluid inclusion characteristics of the Kumbel oxidized W–Cu–Mo skarn and Au–W stockwork deposit in Kyrgyzstan, Tien Shan
Published Date
Feb 1, 2015
Volume
50
Issue
2
Pages
187 - 220
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