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Godula Beds

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Topological architecture of the multiconnected loop topological prototype included in tree graphoglyptids with reservations. A–C, Fossil examples of the multiconnected loop topological prototype. A, Lorenzinia carpathica (Zuber, 1910), Paleocene, Variegated Shale, Lipnica Mała, Carpathians, Poland, UJ TF 134. B, Capodistria vettersi Vialov, 1968, Cenomanian, Lower Godula Beds, Jaroszowice, Carpathians, Poland, UJ TF 96. C, Fascisichnium extentum Książkiewicz, 1968, holotype, Paleocene, Variegated Shale, Lipnica Mała, Carpathians, Poland, UJ TF 1567. D, Topological structures of the multiconnected loop topological prototype.
Published: 06 March 2018
, Carpathians, Poland, UJ TF 134. B, Capodistria vettersi Vialov, 1968 , Cenomanian, Lower Godula Beds, Jaroszowice, Carpathians, Poland, UJ TF 96. C, Fascisichnium extentum Książkiewicz, 1968 , holotype, Paleocene, Variegated Shale, Lipnica Mała, Carpathians, Poland, UJ TF 1567. D, Topological structures
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Topological architecture and prototypes of multiconnected tree graphoglyptids, the multilink linear minor group. A–J, Fossil examples of the multilink linear subgroup of tree graphoglyptids. A, Arabesca simplex (Seilacher, 1977), Eocene, Zarauz, northern Spain, traced from Seilacher (1977: Fig. 9a). B, Arabesca cervicorne (Seilacher, 1977), Eocene, Pindos, Greece, traced from Seilacher (1977: Fig. 9b). C, Ubinia alternans (Seilacher, 1977), Cenomanian, Lower Godula Beds, Wisła, Carpathians, Poland, UJ TF 2726. D, Urohelminthoida dertonensis Sacco, 1888, lower Eocene, Beloveža Formation, Osielec, Carpathians, Poland, UJ TF 141. E, Desmograpton ichthyforme (Macsotay, 1967), note the locally present straight connecting tunnels, Campanian–Paleocene, Ropianka Formation, Lipnica Wielka, Carpathians, Poland, UJ TF 1119. F, Desmograpton alternum (Książkiewicz, 1977), holotype, lower Eocene, Beloveža Formation, Berest, Carpathians, Poland, UJ TF 843. G, Helicolithus tortuosus (Książkiewicz, 1970), note the short, straight connecting tunnels between the S-shaped burrow segments, Eocene, Flysch del Grivo, Vemasso Quarry, NE Italy, 149P5. H, Helicolithus tortuosus (Książkiewicz, 1970), note the additional arc-shaped tunnel, connecting tunnels mostly not preserved, Miocene, Cingöz Formation, southern Turkey (photograph courtesy of Huríye Demírcan), see Demírcan and Toker (2004: Plate 2, Fig. 3). I, Paleomeandron elegans Peruzzi, 1880, Campanian–Paleocene, Ropianka Formation, Lipnica Mała, Carpathians, Poland, UJ TF 220. J, Paleomeandron rude Peruzzi, 1880, middle Eocene, Hieroglyphic Beds, Grzechynia, Carpathians, Poland, UJ TF 138. K, Topological prototypes of the multilink linear subgroup of tree graphoglyptids (a total of three, illustrating the burrow margins of different connected components).
Published: 06 March 2018
( 1977 : Fig. 9 a). B, Arabesca cervicorne (Seilacher, 1977 ), Eocene, Pindos, Greece, traced from Seilacher ( 1977 : Fig. 9 b). C, Ubinia alternans (Seilacher, 1977 ), Cenomanian, Lower Godula Beds, Wisła, Carpathians, Poland, UJ TF 2726. D, Urohelminthoida dertonensis Sacco, 1888 , lower
Journal Article
Published: 01 July 2006
Journal of Foraminiferal Research (2006) 36 (3): 273–275.
.... A: Kraków, Poland, Polsk Akademia Nauk. Studia Geologica Polonica, v. 124, 2005, 410 pages: L emanska , A. Comparison of deep-water agglutinated foraminifera from the hemipelagic variegated shales (Lower Turonian-Lower Santonian) and turbiditic Godula beds (Upper Santonian-Campanian) in the Lanckorona...
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985610M843070
EISBN: 9781629810379
... shales. During the early part of the Late Cretaceous, a supply of clastic material commenced. The uppermost Turonian and the lower Senonian are represented by a very thick flysch series of Godula beds (approximately 2000 m [6600 ft] thick) developed as thick- and thin-bedded sandstones intercalated...
Series: SEPM Special Publication
Publisher: SEPM (Society for Sedimentary Geology)
Published: 01 January 2009
DOI: 10.2110/sepmsp.091.099
EISBN: 9781565762961
... flysch higher in the section. Variegated sediments of the lower member are overlain by thick-bedded medium-to coarse-grained sandstones (the middle member of the Godula Formation). Sandstone beds represent probable fluxoturbidites which are several meters thick. They are interbedded with rhythmic...
Journal Article
Journal: Paleobiology
Published: 06 March 2018
Paleobiology (2018) 44 (2): 306–325.
..., Carpathians, Poland, UJ TF 134. B, Capodistria vettersi Vialov, 1968 , Cenomanian, Lower Godula Beds, Jaroszowice, Carpathians, Poland, UJ TF 96. C, Fascisichnium extentum Książkiewicz, 1968 , holotype, Paleocene, Variegated Shale, Lipnica Mała, Carpathians, Poland, UJ TF 1567. D, Topological structures...
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First thumbnail for: Topological analysis of graphoglyptid trace fossil...
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Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985616M843071
EISBN: 9781629810379
... deposited in basin-floor fans. The main seals in the field are the Verovice shales, Lgota Shales, and the younger Godula Shales and Weglowka marls. Copyright ©2006. The American Association of Petroleum Geologists. DOI:10.1306/985616M843071 Introduction The Weglowka oil field is one of the most...
Journal Article
Published: 01 May 2017
Vadose Zone Journal (2017) 16 (5): 1–9.
... formed during the postglacial period. Other studied wells are located in the village of Jaszczurowa (the Beskid Mały mountains, drainage area of the River Skawa). This area is built on flysch deposits that belong to the Silesian and Sub-Silesian units. The Godula Beds are represented by thin layers...
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First thumbnail for: Patterns of Benthic Fauna Distribution in Wells: T...
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Third thumbnail for: Patterns of Benthic Fauna Distribution in Wells: T...
Journal Article
Journal: PALAIOS
Published: 06 July 2023
PALAIOS (2023) 38 (6): 281–303.
...., 2013 , Coprolite of a durophagous carnivore from the Upper Cretaceous Godula Beds, Outer Western Carpathians : Poland Geological Quarterly , v . 57 , p . 361 – 364 . Bajdek, P., Owocki...
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First thumbnail for: LAURUSSIAN-ASPECT OF THE COPROLITE ASSOCIATION FRO...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1979
AAPG Bulletin (1979) 63 (1): 67–86.
... and sandstone ( Fig. 8A ). Thicker beds of sandstone and conglomerate are distributed mainly in the lower part of the sequence, although some isolated beds appear in the upper part of the section as well ( Fig. 7 ). Fig. 8 —Examples of stratification in upper part of Paleogene canyon fill. A, Laminated...
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First thumbnail for: Ancient Submarine Canyons of Tethyan Continental M...
Second thumbnail for: Ancient Submarine Canyons of Tethyan Continental M...
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Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985605M843071
EISBN: 9781629810379
..., Dziadzio, 2006 ). The Silesian Nappe Within the Subsilesian and the Silesian units, the Lgota beds are overlain by the green shales with intercalation of black shales and radiolarites (Cenomanian) and the Godula beds ( Figure 1 ). Within the northeastern part of the Outer Carpathians, the Godula...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1931
AAPG Bulletin (1931) 15 (1): 1–41.
... in the Western Carpathians and in many places in the Eastern Carpathians, and in the same group are the Audia shales in Roumania. These beds are black shales commonly containing layers of hornstone and of sphero-siderite. Their age is Barremian or Aptian. The Ellgoth formation and the sandstone of Godula occur...
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First thumbnail for: Geology of Oil Fields of Polish Carpathian Mountai...
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Journal Article
Journal: AAPG Bulletin
Published: 15 October 2019
AAPG Bulletin (2019) 103 (10): 2369–2398.
...)-thick beds. These beds are nonarenaceous, soft, and bioturbated. Grain size corresponds to approximately 80% clay and less than 20% silt fractions. X-ray diffraction (XRD) reveals that the marls contain, on average, 54% clay, 28% calcite, 16% quartz, up to 3% feldspars and, in red marls, 3% hematite...
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First thumbnail for: The cap rocks sealing the reservoir in the Węglówk...
Second thumbnail for: The cap rocks sealing the reservoir in the Węglówk...
Third thumbnail for: The cap rocks sealing the reservoir in the Węglówk...
Series: Geological Society, London, Engineering Geology Special Publications
Published: 01 January 2010
DOI: 10.1144/EGSP23.11
EISBN: 9781862393851
...) in the eastern part of the Moravskoslezské Beskydy Mountains (Fig.  1 ). Gently dipping (up to 5°) sandstones of the Godula Formation (single beds 1–5 m thick) form a massive ridge with pronounced structural flats on the watersheds. The Ropice massif is situated at the intersection of three fault structures...
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985629M841463
EISBN: 9781629810379
...     Late Cretaceous flysch (Ropianka), calcareous turbidites marls, radiolarites, green and red shales thick-bedded, coarse-grained turbidites and fluxoturbidites (Godula, Istebna), flysch (Ropianka), marls, (Weglowka,Frydek) Stage I (500–365 Ma) Devonian black shales, cherty limestones, cherts...
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985618M843076
EISBN: 9781629810379
... are Weglowka marls and Godula Shales. Bottom seals are the Weglowka marls (Santonian to Eocene). The complex sealing relationships are caused by tectonic repetition of stratigraphic units in the fold and duplex structures of the Carpathian thrust system. Generally, the tec-tonic structure of the reservoir...
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985607M843067
EISBN: 9781629810379
... of the Silesian ridgein the Cenomanian-Turonian ( Poprawa et al., 2002 ) is documented by the deposition of thick coarse clastics of the Godula and Istebna formations (Cenomanian-Turonian to Paleocene) in the Silesian basin. Only later, since the late Campanian, were the coarse clastics from the Silesian...
Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.3
EISBN: 9781862393899
... ( Wiese et al. 2004a ; Schioler et al. 1997). Tectonic setting The rhythmic bedding of clays and chalk at some levels in the Cretaceous succession is interpreted as reflecting climatic changes within the Milankovitch frequency band (e.g. Gale et al. 1999 ). The bedding commonly shows...
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP465.24
EISBN: 9781786203656
... coarse-grained sandstones (e.g. Grodziszcze, Lgota, Godula, Istebna, Ciężkowice and Kliwa sandstones) form good-quality reservoirs ( Karnkowski 1993 ; Dziadzio et al. 2006 ). Traps are mostly structural, related to various folds formed during emplacement of the Carpathian fold-and-thrust belt...
Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.6
EISBN: 9781862393899
... . In Permian times, fluviatile red-beds (e.g. Prebichl Formation) and, locally, shallow-marine evaporitic sediments were deposited in the area of the three nappe systems. Subsequently, a shallow-marine basin developed, broadly silicilastic-filled with limestone layers intercalated in the upper part (Werfen...