Evolution of the Mo-rich scheelite skarn mineralization at Kozbudaklar, Western Anatolia, Turkey: Evidence from mineral chemistry and fluid inclusions
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- 作者：Ayşe Orhan ; ayse.orhan@nevsehir.edu.tr" class="auth_mail" title="E-mail the corresponding author
- 关键词：Scheelite mineralization ; Fluid evolution ; Kozbudaklar ; Western Anatolia
- 刊名：Ore Geology Reviews
- 出版年：2017
- 出版时间：January 2017
- 年：2017
- 卷：80
- 期：Complete
- 页码：141-165
- 全文大小：6184 K
文摘
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Scheelite mineralization is developed with clinopyroxene and garnet having different compositions in two prograde substages.
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Early scheelite deposition is formed with partly reduced skarn assemblage under moderately reduced oxidized conditions.
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Second scheelite (Mo-rich) deposition took place by oxidizing fluid compositions, probably induced by fluid boiling.
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Fluid inclusions exhibit high temperature and high salinity.