Facies anatomy of a progradational submarine channelized lobe complex: semi-quantitative analysis of the Ropianka Formation (Campanian-Paleocene) in Hucisko Jawornickie section, Skole Nappe, Polish Carpathians

Łapcik, Piotr

doi:10.1515/agp-2018-0026

Artykuł - szczegóły

Tytuł artykułu

Facies anatomy of a progradational submarine channelized lobe complex: semi-quantitative analysis of the Ropianka Formation (Campanian-Paleocene) in Hucisko Jawornickie section, Skole Nappe, Polish Carpathians

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Łapcik Piotr

Treść / Zawartość

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Identyfikatory

DOI

10.1515/agp-2018-0026

Warianty tytułu

Języki publikacji

Abstrakty

This study is a detailed lithofacies analysis of the Wiar and Leszczyny members of the deep-marine Ropianka Formation (Campanian–Paleocene) exposed in the Hucisko Jawornickie section of the Skole Nappe, Polish Carpathian Flysch. The sedimentary succession (>400 m thick) represents a channelized lobe complex that prograded at the base of submarine slope. Seven sedimentary facies are recognized as a record of the principal modes of sediment deposition. Based on their stratigraphic grouping and grain-size trends, six facies associations are distinguished as representing specific sub-environments of the depositional system: distributary channels, channel-mouth lobes, channel levees, crevasses and interlobe basin plain with crevasse splays. The individual facies associations are characterized statistically and their internal facies organization is analysed by the method of embedded Markov chains to reveal the time pattern of depositional processes. The environmental changes indicated by the vertical succession of facies associations are attributed to the autogenic processes of the distributary channel shifting within an aggrading lobe area and the lateral switching of depositional lobes. Eustatic influences are likely, but difficult to ascertain with poor biostratigraphic data. The bulk basinward advance of the base-of-slope system was probably due to a pulse of the tectonic narrowing of the synclinal Skole Basin.

Słowa kluczowe

deep-marine turbidites depositional lobes submarine channels dynamic stratigraphy facies analysis Markov chain analysis

turbidyty loby depozycyjne kanały podmorskie stratygrafia dynamiczna analiza facjalna łańcuch Markova

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2019

Tom

Vol. 69, no. 1

Strony

111--141

Opis fizyczny

Bibliogr. 140 poz., rys., tab.

Twórcy

autor

Łapcik Piotr

piotr.lapcik@doctoral.uj.edu.pl

Jagiellonian University, Institute of Geological Sciences, ul. Gronostajowa 3a, PL-30-387 Kraków, Poland.

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).

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Bibliografia

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