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  5. Mineral Chemistry of Scheelite as An Indicator of Multi-stage Fluid Evolution Associated with the Ri

Mineral Chemistry of Scheelite as An Indicator of Multi-stage Fluid Evolution Associated with the Ri

来源 :11th International Congress of Applied Mineralogy,11thICAM(第 | 被引量 : 0次 | 上传用户：colossus198201
【摘 要】
：
The Neoproterozoic Riviera W-REE-Mo deposit is one of the largest unmined tungsten resources in the world and is associated with pervasively altered A-type gran
【作 者】
：
Abraham Rozendaal Rene Heyn 
【机 构】
：
DepartmentofEarthSciences,UniversityofStellenbosch,Stellenbosch,SouthAfrica
【出 处】
：
11th International Congress of Applied Mineralogy,11thICAM(第
【发表日期】
：
2013年7期
【关键词】
：
mineral chemistry multi-stage fluid evolution scheelite the Riviera W-REE-Mo dep 
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论文部分内容阅读
The Neoproterozoic Riviera W-REE-Mo deposit is one of the largest unmined tungsten resources in the world and is associated with pervasively altered A-type granites of the Neoproterozoic Cape Granite Suite Western Cape, South Africa.The present study investigated the mineral chemistry of scheelite, the principal ore mineral with the aim to record the variation of solid solution molybdenum for geometallurgical purposes and also as an indicator of changing redox conditions of the mineralizing hydrothermal fluids.
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