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- W2000687653 abstract "The Kamyshin ore field incorporates two economic deposits (the Kamyshin and the Artem'yev), that occur in a sequence of gently dipping volcanic, volcanosedimentary, and sedimentary rocks of Middle and Late Devonian age. Late Devonian intrusives play an important role in the structure of the ore field. The main ore-controlling structure is a large stratovolcano of Givetian age, composed of lava flows and rhyolite lava breccias. Ore bodies lie at the base of the elongate apical depression of the stratovolcano and are overlain by basalts and siltstones. The main valuable metals are copper, lead, and zinc. Vertical mineral zoning is clearly evident, from top to bottom: barite-galena-sphalerite with fahlore, pyrite-chalcopyrite-sphalerite, and pyrite-chalcopyrite, both massive and disseminated. Several rare minerals of bismuth, gold, and silver also are important. Geological setting, morphology, ore composition, and conditions of ore deposition suggest that the Kamyshin deposits are of the Kuroko type." @default.
- W2000687653 created "2016-06-24" @default.
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- W2000687653 date "1993-08-01" @default.
- W2000687653 modified "2023-09-27" @default.
- W2000687653 title "MASSIVE SULFIDE-POLYMETALLIC DEPOSITS OF THE KAMYSHIN ORE FIELD, EASTERN KAZAKHSTAN" @default.
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- W2000687653 doi "https://doi.org/10.1080/00206819309465555" @default.
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