Stratigraphic Features of the Yesilova Ophiolite, Burdur, South-Western Turkey

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dc.contributor.authorDoyen, Adnan
dc.contributor.authorComlekciler, Fuat
dc.contributor.authorKocak, Kerim
dc.date.accessioned2020-03-26T18:58:32Z
dc.date.available2020-03-26T18:58:32Z
dc.date.issued2014
dc.departmentSelçuk Üniversitesien_US
dc.description1st International Congress on Stratigraphy (STRATI) -- JUL 01-07, 2013 -- Lisbon, PORTUGALen_US
dc.description.abstractThe Yesilova ophiolite is located in the Alpine zone as a major part of the Lycian nappes of western Taurus. It was formed at the southern branch of Neo-Tethys, and was abducted over the southern edge of the Menderes Massif during the Cenonian during Laramian orogenesis. The ophiolite in the study area starts with tectonite, consisting mainly of harzburgites (37.02 % MgO, 38.77 % SiO2, and 0.42 % Cr2O3) and smaller amounts of dunite and chromite pods. The sequence continues with cumulates, including (from bottom to top) dunite, wehrlite, clinopyroxenite, layered and nonlayered gabbro (45.53 % SiO2, 11.92 % Al2O3, and 13.11 % MgO), and plagiogranite (77.41 % SiO2, 0.25 % K2O). The tectonite and cumulates have been cut by isolated gabbro and diabase dikes. The altered volcanites are found at the top of ophiolitic sequence, and were abducted by the Upper Cretaceous Kizilcadag Melange, with limestone, chert-radiolarite blocks, and ophiolitic rock fragments. The upper Eocene Varsakyayla Formation rests over the melange; it contains abundant nummulites and is composed of conglomerate sandstone, limestone, and conglomerate towards the top. The stratigraphic sequence continues with the Pliocene-Quaternary Niyazlar Formation, consisting of terrigenous conglomerate intercalated with sandstone, and ends with rock talus and alluvium.en_US
dc.description.sponsorshipIUGS, Int Commiss Stratig, New Univ Lisbon, Fac Sci & Technol, Res Ctr Geol Sci & Engn, New Univ Lisbon, Fac Sci & Techno, Dept Earth Sci, GALP Energia SGPS S A, Partex Oil & Gas, Inst Francais Portugal, Centro Investigacao Ciencia & Engn Geologica, New Univ Lisbonen_US
dc.identifier.doi10.1007/978-3-319-04364-7_94en_US
dc.identifier.endpage498en_US
dc.identifier.isbn978-3-319-04364-7; 978-3-319-04363-0
dc.identifier.issn2197-9545en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage493en_US
dc.identifier.urihttps://dx.doi.org/10.1007/978-3-319-04364-7_94
dc.identifier.urihttps://hdl.handle.net/20.500.12395/31155
dc.identifier.wosWOS:000359019400094en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSPRINGER INT PUBLISHING AGen_US
dc.relation.ispartofSTRATI 2013en_US
dc.relation.ispartofseriesSpringer Geology
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectNummulitesen_US
dc.subjectYesilova ophioliteen_US
dc.subjectSalda lakeen_US
dc.subjectTurkeyen_US
dc.titleStratigraphic Features of the Yesilova Ophiolite, Burdur, South-Western Turkeyen_US
dc.typeConference Objecten_US

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