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• W2038768192 startingPage "195" @default.
• W2038768192 abstract "Regional geochemical data from the classic mining districts of Southwest England, the Pennine orefields of Central England, and the Dalradian belt of Scotland, with its important occurrences of gold, are considered as a basis for understanding metallogenic provinces. The deposit types are granite-associated Sn-U, Mississippi Valley Type Pb-Zn-Ba-F and vein Au. It is suggested that crustal reservoirs, enriched in ore-forming elements, were important in the genesis of the examples of Sn-U and Au mineralisation studied. The reservoirs comprise evolved subalkaline granites and carbonaceous sulphur-enriched turbidities in listric faulted orogenic basins, respectively. In the case of the Pennine base-metal deposits, the reservoirs from which the ore-forming fluids were derived, comprise sedimentary basins approximating in composition to average shale and ore deposition mainly reflects the nature of basin evolution. The regional geochemical data used in the study were derived from geochemical atlases produced for different purposes and to different standards. Nevertheless, simple trace-element plots normalised, for example, to average crustal abundances can be used together with geological and geophysical criteria to summarise key characteristics of the crustal reservoirs identified and to develop methods suitable for screening spatially related data sets using Image Analysis or Geographical Information Systems." @default.
• W2038768192 created "2016-06-24" @default.
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• W2038768192 date "1990-12-01" @default.
• W2038768192 modified "2023-10-17" @default.
• W2038768192 title "Regional geochemistry and the identification of metallogenic provinces: examples from lead-zinc-barium, tin-uranium and gold deposits" @default.
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• W2038768192 doi "https://doi.org/10.1016/0375-6742(90)90074-k" @default.
• W2038768192 hasPublicationYear "1990" @default.
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