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dc.contributor.authorGul, Murat
dc.date.accessioned2020-11-20T15:06:56Z
dc.date.available2020-11-20T15:06:56Z
dc.date.issued2015
dc.identifier.issn2391-5447
dc.identifier.urihttps://doi.org/10.1515/geo-2015-0029
dc.identifier.urihttps://hdl.handle.net/20.500.12809/3190
dc.descriptionGul, Murat/0000-0003-1555-6426en_US
dc.descriptionWOS: 000371283800028en_US
dc.description.abstractThe Lycian Nappes, containing ophiolite and sedimentary rocks sequences, crop out in the southwest Turkey. The Tavas Nappe is a part of the Lycian Nappes. It includes the Lower Jurassic-Upper Cretaceous calciturbidites. Chert occurrences were observed in the lower part of this calciturbidite. These cherts can be classified on the basis of length, internal structure and host rock. Chert bands are 3.20-35.0 m in length and 7.0-35.0 cm thick. Chert lenses are 5.0-175.0 cm in length and 1.0-33.0 cm thick. According to its internal structure, granular chert (bladedlarge equitant quartz minerals replaced the big calcite mineral of fossil shell) and porcelanious chert (microcrystalline silica replaced micrite) have been separated. Cherts are generally associated with calcarenite-calcirudite, the others with calcilutite. Micritic calcite patches of cherts point out an uncompleted silicification. The source of silica was dominantly quartz-rich, older, basal rocks and to a lesser extent radiolarians. The coarse-grained calciturbidites act as a way for silica transportation. Some calcite veins (formed during transportation and emplacement of nappes) cut both calciturbidites and cherts. Thus, chert occurrences evolved before emplacement of nappes (the latest Cretaceous-Late Miocene period) during the epigenetic phase.en_US
dc.item-language.isoengen_US
dc.publisherDe Gruyter Open Ltden_US
dc.item-rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectChert Banden_US
dc.subjectChert Lensen_US
dc.subjectRadiolariaen_US
dc.subjectCalciturbiditeen_US
dc.subjectSilicificationen_US
dc.titleOccurrences of Chert in Jurassic-Cretaceous Calciturbidites (SW Turkey)en_US
dc.item-typearticleen_US
dc.contributor.departmenten_US
dc.contributor.departmentTemp[Gul, Murat] Mugla Sitki Kocman Univ, Fac Engn, Dept Geol Engn, TR-48000 Kotekli, Mugla, Turkeyen_US
dc.identifier.doi10.1515/geo-2015-0029
dc.identifier.volume7en_US
dc.identifier.issue1en_US
dc.identifier.startpage446en_US
dc.identifier.endpage464en_US
dc.relation.journalOpen Geosciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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