Geology, mineralization, and fluid inclusion characteristics of the Chorukh-Dairon W-Mo-Cu skarn deposit in the Middle Tien Shan, Northern Tajikistan
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- 作者：Serguei G. Solovieva ; serguei07@hotmail.com" class="auth_mail" title="E-mail the corresponding author ; Sergey Kryazhevb
- 关键词：Garnet skarn ; Scapolite ; Albite ; Tungsten ; Molybdenum ; Fluid inclusions ; Tien Shan ; Central Asia
- 刊名：Ore Geology Reviews
- 出版年：2017
- 出版时间：January 2017
- 年：2017
- 卷：80
- 期：Complete
- 页码：79-102
- 全文大小：4345 K
文摘
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The deposit is an example of the oxidized-type skarn related to high-K to shoshonitic igneous suite.
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Two to three major stages of scheelite and sulfide deposition occurred.
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Fluid evolution included an early high-temperature, high-pressure, and high-salinity homogenous fluid.
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At a later stage, fluid boiling contributed to intense scheelite deposition.
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Fluids have been sourced from crystallizing magma, with progressing admixture of meteoric water.