A 'soft-rock' petroleum-type approach to exploration for 'hard-rock' minerals in sedimentary basins D. Taylor I. Introduction Several major groups of ore deposits are found as tabular, stratiform bodies or as cross cutting but essentially stratabound deposits within sedimentary basins. Important exam ples are oxide and carbonate ores of iron and manganese, copper and zinc-lead sulphides and gold-uranium deposits. Where the host basins have been strongly in verted and deeply eroded and the mineralized horizons brought to outcrop, the laterally extensive nature of the mineralization usually…mehr
A 'soft-rock' petroleum-type approach to exploration for 'hard-rock' minerals in sedimentary basins D. Taylor I. Introduction Several major groups of ore deposits are found as tabular, stratiform bodies or as cross cutting but essentially stratabound deposits within sedimentary basins. Important exam ples are oxide and carbonate ores of iron and manganese, copper and zinc-lead sulphides and gold-uranium deposits. Where the host basins have been strongly in verted and deeply eroded and the mineralized horizons brought to outcrop, the laterally extensive nature of the mineralization usually results in outcrop or subcrop of the ore itself. Direct detection by geological or geochemical prospecting is then possible. Major deposits also occur in basins which have not been strongly deformed and deeply eroded as non-outcropping sub-horizontal sheets (Polish Kupferschiefer deposits of the fore-Sudetic Monocline) or linear belts (Vibumam Trend, Missouri, Admiral Bay, NW Australia). I believe that both the Polish Kupferschiefer and Admiral Bay de posits were found by chance during oil and gas exploration, and deposits of this type are similar in attitude and dimensions to small-medium size oil and gasfields.Hinweis: Dieser Artikel kann nur an eine deutsche Lieferadresse ausgeliefert werden.
Introduction: 'Soft-rock' petroleum-type approach to exploration for 'hard-rock' minerals in sedimentary basins.- I: Processes and Indicators in Organic-Metal Interaction.- 1 Alteration and migration processes of organic matter in hydrothermal systems and implications for metallogenesis.- 2 Paragenesis of gold- and hydrocarbon-bearing fluids in gold deposits.- 3 Trace elements and Sr isotopic composition of waters from the Great Artesian Basin of Australia: Implications for the formation of ore deposits and hydrocarbon resources.- II: Proterozoic Organic-Metal Interactions.- 4 Nature of organic matter in the early Proterozoic, earliest life forms and metal associations.- 5 Organic and mineral matter in a Precambrian shungite deposit from Karelia, Russia.- 6 Influence of basin fill architecture on fluid flow and ore genesis in the Mount Isa Basin, Northern Australia.- 7 Metallogenesis and hydrocarbon generation in northern Mount Isa Basin, Australia; Implications for ore grade mineralization.- III: Palaeozoic: Hydrothermal Systems and Sediment-Hosted Ore Bodies.- 8 Volcanic and post-volcanic hydrothermal activity in the Intrasudetic Basin, SW Poland: Implications for mineralization.- 9 Organic matter and metal enrichment in black shales of the Illinois Basin, USA.- 10 Organic matter from Zechstein copper deposits (Kupferschiefer) in Poland.- 11 Metalloporphyrin composition and a model for the early diagenetic mineralization of the Permian Kupferschiefer, SW Poland.- 12 The carbonate-hosted base-metal sulphide Polaris deposit in the Canadian Arctic: Organic matter alteration and clay diagenesis.- 13 Nature and source of carbonate mineralization in Bowen Basin coals, Eastern Australia.- 14 Minerals in coal.- 15 Mineralization in eastern Australia coals: Afunction of oil generation and primary migration.- IV: Mesozoic to Recent.- 16 Implications of hydrocarbons in gold-bearing epithermal systems: Selected examples from the Canadian Cordillera.- 17 The association of gold-mercury mineralization and hydrocarbons in the coastal ranges of northern California.- 18 Thermal history of selected sedimentary basins in an island arc: evidence from organic matter and fluid inclusions.- 19 Nannobacteria, fiction or fact?.- V.- 20 Summary and Future Directions.
Introduction: 'Soft-rock' petroleum-type approach to exploration for 'hard-rock' minerals in sedimentary basins.- I: Processes and Indicators in Organic-Metal Interaction.- 1 Alteration and migration processes of organic matter in hydrothermal systems and implications for metallogenesis.- 2 Paragenesis of gold- and hydrocarbon-bearing fluids in gold deposits.- 3 Trace elements and Sr isotopic composition of waters from the Great Artesian Basin of Australia: Implications for the formation of ore deposits and hydrocarbon resources.- II: Proterozoic Organic-Metal Interactions.- 4 Nature of organic matter in the early Proterozoic, earliest life forms and metal associations.- 5 Organic and mineral matter in a Precambrian shungite deposit from Karelia, Russia.- 6 Influence of basin fill architecture on fluid flow and ore genesis in the Mount Isa Basin, Northern Australia.- 7 Metallogenesis and hydrocarbon generation in northern Mount Isa Basin, Australia; Implications for ore grade mineralization.- III: Palaeozoic: Hydrothermal Systems and Sediment-Hosted Ore Bodies.- 8 Volcanic and post-volcanic hydrothermal activity in the Intrasudetic Basin, SW Poland: Implications for mineralization.- 9 Organic matter and metal enrichment in black shales of the Illinois Basin, USA.- 10 Organic matter from Zechstein copper deposits (Kupferschiefer) in Poland.- 11 Metalloporphyrin composition and a model for the early diagenetic mineralization of the Permian Kupferschiefer, SW Poland.- 12 The carbonate-hosted base-metal sulphide Polaris deposit in the Canadian Arctic: Organic matter alteration and clay diagenesis.- 13 Nature and source of carbonate mineralization in Bowen Basin coals, Eastern Australia.- 14 Minerals in coal.- 15 Mineralization in eastern Australia coals: Afunction of oil generation and primary migration.- IV: Mesozoic to Recent.- 16 Implications of hydrocarbons in gold-bearing epithermal systems: Selected examples from the Canadian Cordillera.- 17 The association of gold-mercury mineralization and hydrocarbons in the coastal ranges of northern California.- 18 Thermal history of selected sedimentary basins in an island arc: evidence from organic matter and fluid inclusions.- 19 Nannobacteria, fiction or fact?.- V.- 20 Summary and Future Directions.
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