Sea-bottom relief versus differential compaction in ancient platform carbonates : a critical reassessment of an example from Upper Jurassic of the Cracow-Wielun

Matyszkiewicz, J.

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Tytuł artykułu

Sea-bottom relief versus differential compaction in ancient platform carbonates : a critical reassessment of an example from Upper Jurassic of the Cracow-Wielun

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Matyszkiewicz J.

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Relief dna morskiego a zróżnicowana kompakcja w kopalnych platformach węglanowych : krytyczne przeszacowanie przykładu z górnej jury Wyżyny Krakowsko-Wieluńskie

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Abstrakty

The growth of carbonate buildups in the northern, stable shelf of the Tethyan Ocean was the principal factor in the development of diversified sea-bottom relief in the Late Jurassic basin. Reconstruction of this relief has been a matter of numerous controversies. This paper provides an analysis of published data on elevation differences on sea bottom along the SW margin of the Holy Cross Mts. and in the Cracow-Wielun Upland. Moreover, methods of reconstruction of synsedimentary relief are presented. In the Late Oxfordian the elevations on basin floor in the Czestochowa area (Cracow-Wielun Upland) were about 100 meters at most, and were presumably even lower. The largest (over 200 meters) elevation differences of sea-bottom relief existing in the Czestochowa area at the Oxfordian/Kimmeridgian have been postulated when the recently observed differences in thickness between the deposits of carbonate buildup and of equivalent basinal facies were identified as a relief. In fact, different thickness is, in considerable part, an effect of differential compaction.

Wzrost budowli węglanowych na północnym, stabilnym szelfie Tetydy był główną przyczyną powstania urozmaiconego reliefu dna w basenie późnojurajskim. Rekonstrukcja tego reliefu jest przedmiotem licznych kontrowersji. Praca analizuje dane literaturowe o wielkości deniwelacji dna z rejonu SW-obrzeżenia Gór Świętokrzyskich i Wyżyny Krakowsko-Wieluńskiej oraz omawia metodykę rekonstrukcji reliefu synsedymentacyjnego. Deniwelacje dna basenu u schyłku oksfordu w rejonie Częstochowy wynosiły co najwyżej około 100 m a przypuszczalnie były jeszcze mniejsze. Postulowane wcześniej, ponad dwustumetrowe deniwelacje w basenie w rejonie Częstochowy na przełomie oksfordu i kimerydu były oparte na utożsamianiu z deniwelacjami dna aktualnej różnicy miąższości między utworami budowli węglanowej a ekwiwalentnymi jej utworami facji basenowej. Różnica ta jest w znacznej części wynikiem zróżnicowanej podatności osadów na kompakcję.

Słowa kluczowe

sea bottom relief carbonate buildup bedded facies compaction Tethyan shelf Late Jurassic

Wydawca

Polskie Towarzystwo Geologiczne

Czasopismo

Annales Societatis Geologorum Poloniae

Rocznik

1999

Tom

Vol. 69, No. 1-2

Strony

63--79

Opis fizyczny

Bibliogr. 117 poz., fot., rys., tab., wykr.

Twórcy

autor

Matyszkiewicz J.

University of Mining and Metallurgy, Faculty of Geology, Geophysics and Environmental Protection,al. Mickiewicza 30; 30-059 Cracow, Poland, jamat@geol.agh.edu.pl

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