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• W2724646801 abstract "The Central Pontides (Turkey) includes several igneous complexes, which are predominantly Permo-Carboniferous and Middle Jurassic in age. The Çangaldağ Pluton is one of the largest igneous bodies located in the northern Central Pontides, whose age and tectono-magmatic evaluation is important to constrain the geological evolution of the Northern Neotethys. The pluton tectonically overlies the Çangaldağ Metamorphic Complex, which represents an arc–back-arc complex of Middle Jurassic age. The Çangaldağ Pluton consists mainly of non-metamorphic gabbroic diorite, dacite porphyry, and lesser amount of granitic rocks. Geochemically, the various rock types are akin to volcanic arc magmas displaying Th/Nb and light rare earth element/heavy rare earth element enrichments. In-situ U–Pb age results of zircons from dacite porphyry and granite samples yield ages of 161 ± 5 Ma and 170 ± 2 Ma, respectively. Corresponding in-situ average 176Hf/177Hf initial ratios are 0.28287 ± 0.00004 and 0.28213 ± 0.00002 for the dacite porphyry and granite samples, respectively. These results are consistent with derivation from a subduction-modified mantle source. Based on Hf isotope compositions, TDM model ages vary between 624 and 1512 Ma and suggest that the arc magmatism associated with the Çangaldağ Pluton may have involved partial melting of Neoproterozoic/Mesoproterozoic crustal rocks, a common feature in Gondwana-derived terranes. The geochemical, Hf isotope, and geochronological data reported here confirm the presence of a continental arc system during the Middle Jurassic in the Central Pontides, and suggests that the Çangaldağ Pluton formed during northward subduction of the Intra-Pontide branch of the Northern Neotethys." @default.
• W2724646801 created "2017-07-14" @default.
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• W2724646801 date "2017-10-01" @default.
• W2724646801 modified "2023-10-16" @default.
• W2724646801 title "Whole rock geochemistry, Zircon U–Pb and Hf isotope systematics of the Çangaldağ Pluton: Evidences for Middle Jurassic Continental Arc Magmatism in the Central Pontides, Turkey" @default.
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• W2724646801 cites W1906208798 @default.
• W2724646801 cites W1967891107 @default.
• W2724646801 cites W1972770857 @default.
• W2724646801 cites W1973530406 @default.
• W2724646801 cites W1981178684 @default.
• W2724646801 cites W1981207838 @default.
• W2724646801 cites W1993290622 @default.
• W2724646801 cites W1993869433 @default.
• W2724646801 cites W1993927073 @default.
• W2724646801 cites W1996585172 @default.
• W2724646801 cites W1999448338 @default.
• W2724646801 cites W2004724861 @default.
• W2724646801 cites W2004826139 @default.
• W2724646801 cites W2005134752 @default.
• W2724646801 cites W2010527394 @default.
• W2724646801 cites W2011332054 @default.
• W2724646801 cites W2011854336 @default.
• W2724646801 cites W2020973699 @default.
• W2724646801 cites W2023918730 @default.
• W2724646801 cites W2025466944 @default.
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• W2724646801 cites W2039020827 @default.
• W2724646801 cites W2039872199 @default.
• W2724646801 cites W2044175358 @default.
• W2724646801 cites W2045594539 @default.
• W2724646801 cites W2045968877 @default.
• W2724646801 cites W2046325246 @default.
• W2724646801 cites W2048857036 @default.
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• W2724646801 cites W2074440625 @default.
• W2724646801 cites W2080271111 @default.
• W2724646801 cites W2080325016 @default.
• W2724646801 cites W2084150033 @default.
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• W2724646801 cites W2108971421 @default.
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• W2724646801 cites W2142918037 @default.
• W2724646801 cites W2145253730 @default.
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• W2724646801 doi "https://doi.org/10.1016/j.lithos.2017.06.020" @default.
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