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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裹体研究-未来前景如何?

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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regional and target appraisal stages of exploration for hydrothermal mineral deposits, drawing largely on published and unpublished case history examples from Sn-W-Cu-(U-Au)-mineralised and barren granitic rocks.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,世界人口可能达到c。到2050年将达到100亿。为了维持这一增长,对矿产的需求也将明显增加。为了满足这一需求,需要对现有的经济可行的矿床进行连续补充。寻找经济沉积物变得越来越困难,并且需要在21世纪开发新的矿产勘探方法。流体包裹体为我们对各种矿石遗传过程的理解做出了重要贡献,这已被广泛接受。它们作为矿物勘探工具的价值也得到了认可(Roedder,1977; Wilkinson,2001),但是在未来可能发展流体包裹体研究并将其直接用于寻找未发现的矿床的方式和程度尚不确定。 。本文重点研究了流体包裹体在热液矿藏勘探区域和目标评估阶段中作为工具的潜在价值和局限性,主要借鉴了Sn-W-Cu-(U-Au)-矿化和贫瘠的花岗岩。

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