SEDIMENTARY CHARACTERISTICS OF THE DIKMENDEDE FORMATION (ANKARA, TURKEY)

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dc.contributor.authorOzkan, Ali Mujdat
dc.contributor.authorBozdag, Ayla
dc.date.accessioned2020-03-26T18:16:04Z
dc.date.available2020-03-26T18:16:04Z
dc.date.issued2011
dc.departmentSelçuk Üniversitesien_US
dc.description11th International Multidisciplinary Scientific GeoConference -- JUN 20-25, 2011 -- Albena, BULGARIAen_US
dc.description.abstractThe Maastrichtian aged Dikmendede Formation in the Orhaniye (Kazan-Ankara) area formed in a deep-marine environment. The formation consists of alternating green, grey-coloured turbiditic conglomerate, sandstone, shale, claystone and marl. The unit has typical flysch features and has sedimentary structures such as thin/thick bedding, normal graded bedding, erosional surfaces, flute casts, load structures, ball-and-pillow structures, bounce marks, slump structures and numerous biogenic traces. The conglomerates of turbiditic channel fills display clast imbrication and graded bedding. The sandstones of the Dikmendede Formation are mainly made of quartz, plagioclase, alkali feldspar (orthoclase, microcline, sanidine), sedimentary (carbonate, chert, sandstone, shale), metamorphic (micaschist, quartzschist, calcschist, phyllite, gneiss), volcanic rock clasts, mica (muscovite, biotite), heavy minerals (epidote, opaque minerals, glaucophane, piroksen, rutile, turmaline). The sandstones, texturally and mineralogically immature, are cemented by calcite and iron-oxides, in addition to clayey (illite, smectite, chlorite) and in a lesser amount micritic matrix.en_US
dc.description.sponsorshipMinist Env & Water, Bulgarian Acad Sci, Acad Sci Czech Republ, Acad Sci IR Iran, Latvian Acad Sci, Polish Acad Sci, Russian Acad Sci, Serbian Acad Sci & Arts, Slovak Acad Sci, Natl Acad Sci Ukraine, Bulgarian Ind Assoc, Bulgarian Acad Sci, Albena Wellness Destinaten_US
dc.identifier.endpage250en_US
dc.identifier.issn1314-2704en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage245en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/26804
dc.identifier.wosWOS:000307366000033en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherINT SCIENTIFIC CONFERENCE SGEMen_US
dc.relation.ispartof11TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE (SGEM 2011), VOL Ien_US
dc.relation.ispartofseriesInternational Multidisciplinary Scientific GeoConference-SGEM
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectOrhaniyeen_US
dc.subjectDikmendedeen_US
dc.subjectsandstoneen_US
dc.subjectflyschen_US
dc.subjectflute casten_US
dc.titleSEDIMENTARY CHARACTERISTICS OF THE DIKMENDEDE FORMATION (ANKARA, TURKEY)en_US
dc.typeConference Objecten_US

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