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Geochemical exploration in Cornwall and Devon: A review

机译:康沃尔和德文郡的地球化学勘探:回顾

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Cornwall and Devon host some of the most significant metallic mineralization in the UK and were an obvious location for geochemical research. Professor John Stuart Webb (1920-2007) and his Applied Geochemistry Research Group at Imperial College, London, provided a framework for much exploration through the 'Wolfson Geochemical Atlas of England and Wales', as well as a number of related projects. The regional geochemistry was followed-up by a number of commercial and government surveys, mainly using residual soils. These have validated many of the techniques developed at Imperial College although no new mines have resulted. Surveys around the Wheal Jane mine and north of the St. Austell granite have located new areas of mineralization associated with the main phase of vein formation, as well as tourmaline-rich breccias and calc-silicates. The distribution of pathfinder elements for Sn and W deposits is erratic and As enrichment appears to be related to distinct host sediments and granite phases. Base metal exploration has defined areas of enrichment within lower Carboniferous sediments, which were detected in the early Imperial College surveys. Deep overburden sampling defined drill targets which intersected sub-economic mineralization. Gold exploration defined a number of targets which appeared largely to be the result of a number of phases of heavy mineral concentration. An exception was low-grade mineralization in Permian volcanic rocks. Very little work has been done on the subsurface signature of the deposits and their relation to the differing granites. This, which was partly the focus of Webb's early work, is a priority for further study.
机译:康沃尔郡和德文郡拥有英国一些最重要的金属矿化区,是进行地球化学研究的明显地点。约翰·斯图尔特·韦伯(John Stuart Webb)教授(1920-2007)及其伦敦帝国学院的应用地球化学研究小组,通过“英格兰和威尔士的沃尔夫森地球化学地图集”以及许多相关项目,为许多探索提供了框架。区域性地球化学之后,进行了许多商业和政府调查,主要使用残留土壤进行了调查。这些都证实了帝国理工学院开发的许多技术,尽管没有新的地雷产生。在Wheal Jane矿山和圣奥斯特尔花岗岩以北的勘测中,发现了与矿脉形成的主要阶段有关的新矿化区域,以及富含电气石的角砾岩和钙硅酸盐。 Sn和W矿床的探路元素分布不规则,并且As富集似乎与明显的基质沉积物和花岗岩相有关。贱金属勘探在较低的石炭纪沉积物中确定了富集区域,这是在帝国学院早期的调查中发现的。深层覆盖层采样确定了与次经济成矿相交的钻探目标。金矿勘探确定了许多目标,这些目标似乎主要是由于大量矿物质浓缩阶段的结果。一个例外是二叠纪火山岩中的低品位矿化。关于矿床的地下特征及其与不同花岗岩的关系的研究很少。这是韦伯早期工作的重点之一,是进一步研究的重点。

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