Petrology of Quaternary volcanic rocks and related plutonic xenoliths from Gölcük volcano, Isparta Angle, Turkey: Origin and evolution of the high-K alkaline series
作者: Bernard PlatevoetÖmer ElitokHervé GuillouJacques-Marie BardintzeffFuzuli YagmurluSébastien NomadeAndré PoissonCatherine DenielNevzat Özgür
作者单位: 1Univ Paris-Sud, Laboratoire GEOPS, UMR CNRS 8148, Bât. 504, F-91405 Orsay, France
2Süleyman Demirel University, Department of Geothermal Energy et Mineral Ressources, Merkez Campus 32260, Isparta, Turkey
3Laboratoire des Sciences du Climat et de l’Environnement (UMR 8212 CEA-CNRS-UVSQ), L’Orme des Merisiers, F-91191 Gif-sur-Yvette, France
4Univ Cergy-Pontoise, ESPE, F-95000 Cergy-Pontoise, France
5Laboratoire Magmas et Volcans, Clermont Université, Univ Blaise Pascal, BP 10448, F-63000 Clermont-Ferrand, France
6CNRS, UMR 6524, LMV, F-63038 Clermont-Ferrand, France
7IRD, R 163, LMV, F-63038 Clermont-Ferrand, France
刊名: Journal of Asian Earth Sciences, 2014, Vol.92 , pp.53-76
来源数据库: Elsevier Journal
DOI: 10.1016/j.jseaes.2014.06.012
关键词: Alkaline magmatismXenolithMantle sourceCarbonatiteMetasomatized lithosphereTurkey
英文摘要: Abstract(#br)The Quaternary volcanism of Isparta, south-western Anatolia, belongs to the post-collisional alkali-potassic to ultrapotassic magmatism, active since Miocene, from Afyon to Isparta. In the so-called Isparta Angle, the magmatism is contemporaneous with the Aegean extensional regime initiated during the Late Miocene and active throughout the Pliocene and Quaternary. The Gölcük volcano-forming stages consist of three main eruptive cycles: Cycle I comprising 200m-thick pyroclastic flow deposits; Cycle II consisting of tephriphonolitic lava dome-flows extruded throughout the caldera; and Cycle III characterized by tuff-ring deposits related to the last phreatoplinian events. These late explosive events sampled plutonic xenoliths that allow to better constrain...
全文获取路径: Elsevier  (合作)
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影响因子:2.379 (2012)

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