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Fluid inclusion studies in mineral exploration - prospects for the future?

机译:矿物勘探中的流体包容性研究 - 未来的前景?

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Recent studies predict that the world's population is likely to reach c. 10 billion by 2050. In order to sustain this growth it is also apparent that demand for minerals will increase. A continuous process of replenishment of economically-viable mineral deposits, as existing ones are worked out, is needed to meet this demand. Economic deposits are becoming increasingly difficult to find and new approaches to mineral exploration need to be developed into the 21st century. It is widely accepted that fluid inclusions have made a major contribution to our understanding of various ore genetic processes. Their value as tools in mineral exploration has also been recognised (Roedder, 1977; Wilkinson, 2001), but the manner and extent to which fluid inclusion studies may be developed in the future and directly applied in the search for undiscovered mineral deposits is less certain. This paper focuses on the potential value and limitations of fluid inclusions as tools in the regional and target appraisal stages of exploration for hydrothermal mineral deposits, drawing largely on published and unpublished case history examples from Sn-W-Cu-(U-Au)-mineralised and barren granitic rocks.
机译:最近的研究预测世界的人口可能达到C.到2050年,100亿美元。为了维持这种增长,这也显而易见的是,对矿物质的需求将增加。需要持续加入经济可行的矿物沉积物,因为现有的矿物沉积物需要解决这一需求。经济存款越来越难以找到和新的矿物勘探方法需要发展到21世纪。众所周知,流体夹杂物对我们对各种矿石遗传过程的理解作出了重大贡献。它们作为矿物勘探工具的价值也得到了认可(罗德德,1977年;威尔金森,2001),但流体包容性研究的方式和范围可以在未来开发,直接应用于未被发现的矿物沉积物不太确定。本文重点介绍了流体包裹物的潜在价值和局限性,作为水热矿床勘探的区域和目标评估阶段的工具,主要是来自SN-W-CU-(U-AU)的公布和未发表的案例历史例子 - 矿化和贫瘠的花岗岩岩石。

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