Petrographic and geochemical characteristics of dolomites of Ki{dotless}zi{dotless}loren formation (Konya, Turkey)

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dc.contributor.authorDinc S.
dc.contributor.authorOrhan H.
dc.date.accessioned2020-03-26T17:29:02Z
dc.date.available2020-03-26T17:29:02Z
dc.date.issued2008
dc.departmentSelçuk Üniversitesien_US
dc.description8th International Scientific Conference on Modern Management of Mine Producing, Geology and Environmental Protection, SGEM 2008 -- 16 June 2008 through 20 June 2008 -- Albena -- 101476en_US
dc.description.abstractThe Upper Triassic-Lower Jurassic Ki{dotless}zi{dotless}loren formation outcroping around the Ki{dotless}zi{dotless}loren mountain, 40 km to the west of Konya begin with dolomite at the base and, grades upward into calcitic dolomite, dolomitic limestone and limeston,. Dolomites are two types; mimetic and non-mimetic. In mimetic dolomit, pellet fossils, ooid and intraclast were poartially or totaly preserved. In non-mimetic dolomite, the depositional texture were totaly destroyed. It is composed of euhedral, hemihedral, dirty-brownish coloured, non zoned and fine to coarse dolomite crystals with linear and intended crsytal boundaries. The CaCO3, MgCO3 ratios and Sr, Mn, Fe content of dolomites are determined as % 53-61mol, % 39-47 mol and 65-171 ppm, 3-37 ppm, % 0,01-0,12 respectively. Having a MgCO3 ratio close to % 50 and a low Sr content are interpreted as the dolomite in the study area was approached to the stoichiometric dolomite. The Sr+2/Ca+2 ratio of dolomitization solution was calculated as having a range between 0,023-0,066. This is higher than present day sea water, and can be interpreted as either the Sr+2/Ca+2 ratio of oceanwater when Ki{dotless}zi{dotless}loren formation formed was higher than today seawater or unsufficient removal of Sr in diagenetic environment during transformation processes of aragonitic limestone to dolomite.en_US
dc.identifier.endpage174en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage165en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/22898
dc.identifier.volume1en_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.relation.ispartof8th International Scientific Conference on Modern Management of Mine Producing, Geology and Environmental Protection, SGEM 2008en_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectDolomiteen_US
dc.subjectKi{dotless}zi{dotless}loren formationen_US
dc.subjectMimetic dolomiteen_US
dc.subjectNon-mimetic dolomiteen_US
dc.titlePetrographic and geochemical characteristics of dolomites of Ki{dotless}zi{dotless}loren formation (Konya, Turkey)en_US
dc.typeConference Objecten_US

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