Seismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland

The Upper Cretaceous complex in the central part of the Carpathian Foreland (southern Poland) is relatively poorly recognized and described. Its formations can be classified as unconventional reservoir due to poor reservoir properties as well as a low recovery factor. The main aim of the article is...

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Autores principales:	Andrzej Urbaniec, Anna Łaba-Biel, Anna Kwietniak, Imoleayo Fashagba
Formato:	article
Lenguaje:	EN
Publicado:	MDPI AG 2021
Materias:	Upper Cretaceous seismic sequence stratigraphy seismic attributes Wheeler diagram Technology T
Acceso en línea:	https://doaj.org/article/96d7a29f03f0461dbf85bea3e6e6cfc9
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spelling	oai:doaj.org-article:96d7a29f03f0461dbf85bea3e6e6cfc92021-11-25T17:28:41ZSeismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland10.3390/en142277761996-1073https://doaj.org/article/96d7a29f03f0461dbf85bea3e6e6cfc92021-11-01T00:00:00Zhttps://www.mdpi.com/1996-1073/14/22/7776https://doaj.org/toc/1996-1073The Upper Cretaceous complex in the central part of the Carpathian Foreland (southern Poland) is relatively poorly recognized and described. Its formations can be classified as unconventional reservoir due to poor reservoir properties as well as a low recovery factor. The main aim of the article is to expand knowledge with conclusions resulting from the analysis of the latest seismic data with the application of seismic sequence stratigraphy. Moreover, the seismic attributes analysis was utilized. The depositional architecture recognition based on both chronostratigraphic horizons and Wheeler diagram interpretations was of paramount importance. A further result was the possibility of using the chronostratigraphic image for tectonostratigraphic interpretation. Two distinguished tectonostratigraphic units corresponding to megasequences were recognized. A tectonic setting of the analyzed interval is associated with global processes noticed by other authors in other parts of the central European Late Cretaceous basin, but also locally accompanied by evidence of small-scale tectonics. This study fills the gap on the issue of paleogeography in the Late Cretaceous sedimentary basin of the Carpathian Foreland. It presents the first results of detailed reconstruction of the basin paleogeography and an attempt to determine the impact of both eustatic and tectonic factors on sedimentation processes.Andrzej UrbaniecAnna Łaba-BielAnna KwietniakImoleayo FashagbaMDPI AGarticleUpper Cretaceousseismic sequence stratigraphyseismic attributesWheeler diagramTechnologyTENEnergies, Vol 14, Iss 7776, p 7776 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Upper Cretaceous seismic sequence stratigraphy seismic attributes Wheeler diagram Technology T
spellingShingle	Upper Cretaceous seismic sequence stratigraphy seismic attributes Wheeler diagram Technology T Andrzej Urbaniec Anna Łaba-Biel Anna Kwietniak Imoleayo Fashagba Seismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland
description	The Upper Cretaceous complex in the central part of the Carpathian Foreland (southern Poland) is relatively poorly recognized and described. Its formations can be classified as unconventional reservoir due to poor reservoir properties as well as a low recovery factor. The main aim of the article is to expand knowledge with conclusions resulting from the analysis of the latest seismic data with the application of seismic sequence stratigraphy. Moreover, the seismic attributes analysis was utilized. The depositional architecture recognition based on both chronostratigraphic horizons and Wheeler diagram interpretations was of paramount importance. A further result was the possibility of using the chronostratigraphic image for tectonostratigraphic interpretation. Two distinguished tectonostratigraphic units corresponding to megasequences were recognized. A tectonic setting of the analyzed interval is associated with global processes noticed by other authors in other parts of the central European Late Cretaceous basin, but also locally accompanied by evidence of small-scale tectonics. This study fills the gap on the issue of paleogeography in the Late Cretaceous sedimentary basin of the Carpathian Foreland. It presents the first results of detailed reconstruction of the basin paleogeography and an attempt to determine the impact of both eustatic and tectonic factors on sedimentation processes.
format	article
author	Andrzej Urbaniec Anna Łaba-Biel Anna Kwietniak Imoleayo Fashagba
author_facet	Andrzej Urbaniec Anna Łaba-Biel Anna Kwietniak Imoleayo Fashagba
author_sort	Andrzej Urbaniec
title	Seismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland
title_short	Seismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland
title_full	Seismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland
title_fullStr	Seismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland
title_full_unstemmed	Seismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland
title_sort	seismostratigraphic interpretation of upper cretaceous reservoir from the carpathian foreland, southern poland
publisher	MDPI AG
publishDate	2021
url	https://doaj.org/article/96d7a29f03f0461dbf85bea3e6e6cfc9
work_keys_str_mv	AT andrzejurbaniec seismostratigraphicinterpretationofuppercretaceousreservoirfromthecarpathianforelandsouthernpoland AT annałababiel seismostratigraphicinterpretationofuppercretaceousreservoirfromthecarpathianforelandsouthernpoland AT annakwietniak seismostratigraphicinterpretationofuppercretaceousreservoirfromthecarpathianforelandsouthernpoland AT imoleayofashagba seismostratigraphicinterpretationofuppercretaceousreservoirfromthecarpathianforelandsouthernpoland
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Seismostratigraphic Interpretation of Upper Cretaceous Reservoir from the Carpathian Foreland, Southern Poland

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