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- W70873114 abstract "Volcano-plutonic belts (VPB) that host porphyry-copper deposits are grouped into basaltic and andesitic types. Basaltic (eugeosynclinal) VPB give rise to island-arc barrier zones (fore-arc). Andesitic VPB originate in an orogenic-activation regime and, depending on the character of the basement, are sub-divided into epicratonic, epimiogeosynclinal, and epieugeosynclinal types. Ore genesis products within the VPB are consistent with vertical and lateral-temporal metallogenic zoning (MZ). In basaltic VPB, copper and gold porphyry-copper deposits are associated with copper massive sulfide ores and are replaced in time by veined polymetallic, and in places, skarn mineralization. MZ of andesitic VPB is controlled by metallogeny of their basement combined with molybdenum-, copper-molybdenum porphyry, and molybdenum-copper deposits (depending on the substratum) as well as with later porphyry Sn, Sn—W, W—Mo, W, Au—Ag ores. The metallogenic style of the VPB is determined by the formation of porphyry deposits. The metallogenic zoning of the VPB is exemplified in some provinces of the Soviet Union." @default.
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- W70873114 date "1986-01-01" @default.
- W70873114 modified "2023-09-25" @default.
- W70873114 title "Metallogenic Zoning of Volcano-Plutonic Belts and Porphyry-Copper Mineralization" @default.
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- W70873114 doi "https://doi.org/10.1007/978-3-642-70902-9_17" @default.
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