Isotopic composition of dolomite associated with Middle Miocene Badenian anhydrites in the Carpathian Foredeep Basin of SE Poland

• Autorzy: Jasionowski M. , Peryt T.M.
• Języki publikacji: EN

Abstrakty

EN

Dolomite is a quite common, although usually minor, constituent of the Badenian sulphate deposits of the Carpathian Foredeep Basin. In the autochthonous member of the Wola Różaniecka 7 borehole (SE Poland) which contains well preserved, large anhydritic pseudo-morphs after selenitic gypsum, dolomite constitutes up to 75% of the rock volume, the rest being anhydrite. Dolomites mostly show peloidal clotted microfabrics typical of microbialites and are interpreted as products of microbially induced precipitation and/or dolomitisation at temperatures around 40°C (as interpreted from the d^18131813

Słowa kluczowe

EN

Middle Miocene; Paratethys; dolomite; anhydrite; carbon and oxygen isotopes; strontium isotopes

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2010
• Tom: Vol. 54, No 4
• Strony: 533--548
• Opis fizyczny: Bibliogr. 32 poz., rys., tab., wykr.

Twórcy

autor

Jasionowski M.

autor

Peryt T.M.

• Polish Geological Institute - National Research Institute, Rakowiecka 4, PL-00-975 Warszawa, Poland,

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