Geochemical and foraminiferal records of environmental changes during the Zechstein Limestone (Lopingian) deposition in Northern Poland

• Autorzy: Peryt M. , Peryt D.
• Języki publikacji: EN

Abstrakty

EN

The entire Zechstein Limestone section of the Zdrada IG 8 borehole (Northern Poland) is composed of oncoid packstone that is accompanied by stromatolites in the upper part of the unit. Deposition of the Zechstein Limestone occurred in persistently subtidal environments, above the storm wave base, in mostly dysoxic conditions, and thus these conditions did not differ essentially from those characteristic for the Kupferschiefer strata. The previous supposition of vadose diagenesis is not confirmed by the isotopic study of calcite that showed its clearly marine values (average d¹³¹⁸

Słowa kluczowe

EN

geochemistry; Poland; carbon and oxygen isotopes; foraminifers; Zechstein Limestone

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2012
• Tom: Vol. 56, No 1
• Strony: 187--198
• Opis fizyczny: Bibliogr. 70 poz., rys., wykr.

Twórcy

autor

Peryt M.

autor

Peryt D.

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

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