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- W2182763431 abstract "The East Pontic metallotect represents a Jurassic to Miocene island arc system, hosting a great number of stratabound base metal deposits (i.e. Murgul, Madenkoy, and Lahanos). These deposits occur in a 150 to 300 m thick strongly altered Upper Cretaceous pyroclastic host rocks. The mineralization is related to the first stage phyllic and argillic alteration and the second stage silicic alteration. The first stage alteration is associated with poor mineralization of disseminated pyrite and chalcopyrite(type i). By comparison, the second stage hydothermal activity is characterized by silicic alteration which contains the commercial ore (types ii and iii). Genetically, the mineralization at Murgul in the eastern part of the East Pontic metallotect is assigned to be subvolcanic-hydrothermal origin whereas the deposits at Madenkoy and Lahanos in the western part of the East Pontic metallotect are genetically associated with a submarine hydrothermal activity in a volcano-sedimentary sequence related to island arc volcanism. The Murgul deposit migt be interpreted as a transitional type tending to porphyry copper deposits (Murgul type). By comparasion the deposits at Lahanos and Madenkoy are Kuroko-type deposits." @default.
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- W2182763431 date "1993-01-01" @default.
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- W2182763431 title "Volcanogenic Massive Sulfide Deposits in the East Pontic Metallotect, NE Turkey" @default.
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