© 2015, Springer-Verlag Berlin Heidelberg.Abstract: The mineral composition proportions of carbonate rocks of Kazanian (Mid-Permian) age in the Petchischi region (eastern part of the Russian Platform) was identified by X-ray powder diffraction, ICP-MS and optical microscopy. The Lower Kazanian deposits are presented predominantly by bio-dolomicrites with changing terrigenous component and the lack of gypsum-bearing layers in the succession. Dolomicrites are prevalent in the Upper Kazanian succession, which is composed of alternation of gypsum-bearing dolomites, clayey dolomites and pure dolomites. The discovered bentonite-bearing component in marls and bentonite clays are proposed as evidence of volcanic activity in the Urals in the Kazanian stage. Two marine facies on the Eastern Russian Platform in the Kazanian: peritidal shallow flat and coastal sabkha agree well with the trends of δ18O and δ13C ratios

Zorina S.

Carbonates and Evaporites

Kazan Federal University Digital Repository

Mineralogical composition of the Lower and Upper Kazanian (Mid-Permian) rocks and facies distribution at the Petchischi region (Eastern Russian Platform)

Carbonates and Evaporites 2017 vol.32 N1, pages 27-43Mineralogical composition of the Lower and UpperKazanian (Mid-Permian) rocks and facies distribution atthe Petchischi region (Eastern Russian Platform)Zorina S.Kazan Federal University, 420008, Kremlevskaya 18, Kazan, RussiaAbstract© 2015, Springer-Verlag Berlin Heidelberg.Abstract: The mineral composition proportions ofcarbonate rocks of Kazanian (Mid-Permian) age in the Petchischi region (eastern part of theRussian Platform) was identified by X-ray powder diffraction, ICP-MS and optical microscopy. TheLower  Kazanian  deposits  are  presented  predominantly  by  bio-dolomicrites  with  changingterrigenous component and the lack of gypsum-bearing layers in the succession. Dolomicritesare prevalent in the Upper Kazanian succession, which is composed of alternation of gypsum-bearing dolomites,  clayey dolomites  and pure dolomites.  The discovered bentonite-bearingcomponent in marls and bentonite clays are proposed as evidence of volcanic activity in theUrals in the Kazanian stage. Two marine facies on the Eastern Russian Platform in the Kazanian:peritidal shallow flat and coastal sabkha agree well with the trends of δ18O and δ13C ratios.http://dx.doi.org/10.1007/s13146-015-0272-3KeywordsDepositional model, Dolomite, Kazanian, Middle Permian, Russian Platform, SabkhaReferences[1] Atabey E (1995) Petrography and origin of dolomites of Yaniktepe Formation (Upper Cretaceous) in GürünAutochthonous, Eastern Turkey. Miner Res Explor Bull 117:59–67[2] Badiozamani K (1973) The Dorag dolomitization model—application to the Middle Ordovician of Wisconsin. JSediment Petrol 43(4):965–984[3] Balabanov YuP,  Burov BV (1998)  Paleomagnetic  characteristics.  In:  Burov BV,  Gubareva VS (eds)  UpperPermian stratotypes and reference sections of the Kazan Region. 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Mineralogical composition of the Lower and Upper Kazanian (Mid-Permian) rocks and facies distribution at the Petchischi region (Eastern Russian Platform)

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