Zechstein (Ca1) limestone-marl alternations from the North-Sudetic Basin, Poland: depositional or diagenetic rhythms?

Biernacka, J.; Borysiuk, K.; Raczyński, P.

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Tytuł artykułu

Zechstein (Ca1) limestone-marl alternations from the North-Sudetic Basin, Poland: depositional or diagenetic rhythms?

Autorzy

Biernacka J. , Borysiuk K. , Raczyński P.

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Abstrakty

Limestone-marl alternations constitute a characteristic rock facies within the Zechstein Limestone (Ca1) deposits of the North-Sudetic Basin, Poland. Rhythmites of this type are exposed in a 10-metres section at Nowy Kooeciół, which from the beginning of the last century has been considered representative for this part of the Zechstein basin, and were formerly interpreted as calcareous storm sediments alternating with marls deposited during more quiet conditions. Our results of sedimentological, petrographical and chemical studies suggest that the Nowy Kościół section is a record of distal storm deposits, but that the present-day layering does not precisely reflect the depositional rhythm. Post-depositional changes have overprinted and blurred the original pattern.We propose a model of diagenetic alteration in which dissolution and reprecipitation of calcium carbonate in the shallow subsurface formed new layer boundaries; subsequent modifications during deeper burial followed these early diagenetic changes.

Słowa kluczowe

Zechstein limestone-marl alternations storm deposits carbonate diagenesis

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2005

Tom

Vol. 49, No. 1

Strony

1--14

Opis fizyczny

Bibliogr. 60 poz., rys., tab., wykr.

Twórcy

autor

Biernacka J.

julbier@amu.edu.pl

Institute of Geology, Adam Mickiewicz University, Maków Polnych 16, PL-61-686 Poznań

autor

Borysiuk K.

Poznań Radiocarbon Laboratory, Rubie¿ 46, PL-61-612 Poznań

autor

Raczyński P.

pracz@ing.uni.wroc.pl

Institute of Geological Sciences, Wrocław University, M. Borna 9, PL-50-204 Wrocław

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