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- W2143481796 abstract "article i nfo Ar/ 39 Ar geochronology New geochemical and 40 Ar/ 39 Ar age data are presented from the Neogene volcanic units of the Karaburun Peninsula, the westernmost part of Western Anatolia. The volcanic rocks in the region are associated with Neogene lacustrine deposition and are characterized by (1) olivine-bearing basaltic-andesites to shoshonites (Karaburun volcanics), high-K calc-alkaline andesites, dacites and latites (Yaylakoy, Armagandag and Kocadag volcanics) of ~16-18 Ma, and (2) mildly-alkaline basalts (Ovacik basalt) and rhyolites (Urla volcanics) of ~11- 12 Ma. The first group of rocks is enriched in LILE and LREE with respect to the HREE and HFSE on N-MORB- normalisedREEandmulti-element spiderdiagrams.Theyarecomparablegeochemicallywithvolcanicrocksin the surrounding regions such as Chios Island and other localities in Western Anatolia. The Ovacik basalt is geochemicallysimilar tothe firststageearly-middleMiocene volcanicrocksbutdiffers fromNWAnatolianlate Miocene alkali basalts. Trace element models indicate that the Kocadag and Armagandag volcanics were produced from the Yaylakoy volcanics by assimilation and fractional crystallization (AFC). Melting models of several trace elements of the most primitive mafic volcanics indicate that their source was metasomatized by subduction-related fluids and was amphibole-bearing garnet-lherzolitic." @default.
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- W2143481796 date "2009-08-01" @default.
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- W2143481796 title "Geochemistry and 40Ar/39Ar geochronology of Miocene volcanic rocks from the Karaburun Peninsula: Implications for amphibole-bearing lithospheric mantle source, Western Anatolia" @default.
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- W2143481796 doi "https://doi.org/10.1016/j.jvolgeores.2009.05.016" @default.
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