PETROGRAPHIC AND GEOCHEMICAL CHARACTERISTICS OF DOLOMITES OF KIZILOREN FORMATION (KONYA, TURKEY)

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dc.contributor.authorDinc, Salih
dc.contributor.authorOrhan, Hukmu
dc.date.accessioned2020-03-26T17:27:26Z
dc.date.available2020-03-26T17:27:26Z
dc.date.issued2008
dc.departmentSelçuk Üniversitesien_US
dc.description8th International Scientific Conference on Modern Management of Mine Producing, Geology and Environmental Protection -- JUN 16-20, 2008 -- Sofia, BULGARIAen_US
dc.description.abstractThe Upper Triassic-Lower Jurassic Kiziloren formation outcroping around the Kiziloren mountain, 40 kin 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 totally 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 CaCO(3), MgCO(3) ratios and Sr, Mn, Fe content of dolomites are determined as % 53-61 mol, % 39-47 mol and 65-171 ppm, 3-37 ppm, % 0,01-0,12 respectively. Having a MgCO(3) 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 Kiziloren 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.endpage173en_US
dc.identifier.isbn978-954-91818-1-4
dc.identifier.startpage165en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/22564
dc.identifier.wosWOS:000275795400022en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.language.isoenen_US
dc.publisherINT SCIENTIFIC CONFERENCE SGEMen_US
dc.relation.ispartofSGEM 2008: 8TH INTERNATIONAL SCIENTIFIC CONFERENCE, VOL I, CONFERENCE PROCEEDINGS: MODERN MANAGEMENT OF MINE PRODUCING GEOLOGY AND ENVIRONMENTAL PROTECTIONen_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.subjectmimetic dolomiteen_US
dc.subjectnon-mimetic dolomiteen_US
dc.subjectKiziloren formationen_US
dc.titlePETROGRAPHIC AND GEOCHEMICAL CHARACTERISTICS OF DOLOMITES OF KIZILOREN FORMATION (KONYA, TURKEY)en_US
dc.typeConference Objecten_US

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