2002
DOI: 10.1007/bf03176485
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Sedimentology of the Miocene evaporitic succession in the north of Çankiri-Çorum basin, central Anatolia, Turkey

Abstract: The upperMiocenenon-marine sedimentsof theCankiri-Corum basinincentralAnatolia, havebothevaporitic andnon-evaporitic successions. Thesesedimentsweredepositedin an evaporiticlake whichhad temporaryepisodesof palustrineconditionsinresponseto seasonal orclimaticchanges. The successionsshowdifferentfaciessuch as sulfates,carbonatesandsiliciclastics. Thesulfatescompriseprimary.reworked anddiageneticgypsum. Theprimarydepositsarepredominantlylaminated gypsum,beddedgypsumandselenite. Thereworked(detrital) gypsum compr… Show more

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Cited by 23 publications
(15 citation statements)
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“…2 Streams and settlements on the relief map of the Tatlicay basin Hakyemez et al 1986;Tuysuz and Dellaoglu 1992;Karadenizli 1999;Kaymakci 2000;Varol et al 2002;Kaymakci et al 2003;Karadenizli et al 2003;Esat 2004;Ozcan et al 2007;Seyitoglu et al 2009) and is well known by most of the researchers in Turkey. The Cankiri basin is a young peripheral molasse basin that surrounds the amalgamated tectonic mosaic of the Pontides (tectonic unit list along with northern border) and the Kırsehir massif (central Turkey).…”
Section: Climate Water Resources and Water Usementioning
confidence: 90%
“…2 Streams and settlements on the relief map of the Tatlicay basin Hakyemez et al 1986;Tuysuz and Dellaoglu 1992;Karadenizli 1999;Kaymakci 2000;Varol et al 2002;Kaymakci et al 2003;Karadenizli et al 2003;Esat 2004;Ozcan et al 2007;Seyitoglu et al 2009) and is well known by most of the researchers in Turkey. The Cankiri basin is a young peripheral molasse basin that surrounds the amalgamated tectonic mosaic of the Pontides (tectonic unit list along with northern border) and the Kırsehir massif (central Turkey).…”
Section: Climate Water Resources and Water Usementioning
confidence: 90%
“…In such an environment, the main source of the Ca 2þ and SO 4 2À may be the Miocene seawater under subtropical climate conditions based on the paleoclimatological reconstructions of the Oligocene-Miocene sediments, conducted by Sancay (2005). The massive gypsum rocks are not widely exposed around the region but they can be attributed to deeper parts of the Aş kale subbasin and continuous anhydrite-gypsum precipitation (e.g., Hardie, 1984;Varol et al, 2002). Overlained nodular, nodular-bedded and laminated microcrystalline gypsum may imply development of a coastal sabkha by being desiccated or filled of lagoon or saline (e.g., Hardie and Eugster, 1971;Schreiber et al, 1976).…”
Section: Depositional Environment Of the As¸kale Formationmentioning
confidence: 98%
“…Messinian evaporates are restricted to the southern part of Turkey and are exposed in the İskenderun-Hatay and Adana basins (Tekin et al 2010;Ilgar et al 2013). Terrestrial evaporates accumulated in the Ç ankırı-Ç orum, Sivas and Tuz Gölü basins during the Tertiary following deposition of marine evaporates (Varol et al 2002;Tekin et al 2001;Gundogan et al 2005;Ayyıldız et al 2009). In contrast, certain central and western Anatolian Miocene basins, such as the Beypazarı, Emet, Bigadiç and Sultançayır basins, are characterized by trona (older) and borate deposited in hydrothermal-induced lake environments (e.g., Ortí et al 1998;Helvacı and Orti 1998;Gündogan and Helvacı 2001;García-Veigas et al 2010;García-Veigas and Helvaci 2013).…”
Section: Introductionmentioning
confidence: 94%