1-19 OF 19 RESULTS FOR

Godula Beds

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
×Close Modal
Sort by
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985616M843071
EISBN: 9781629810379
... of the Lgota beds exceeds 650m (2130ft). The thickness of the Godula Shalesranges from a few meters adjacent to the thrust faults (e.g., in the southeast and northwest parts of the Weglowka oil field) to about 100 m (330 ft) in the central part of the field. The youngest deposits are the Weglowka marls...
FIGURES | View All (5)
Series: SEPM Special Publication
Published: 01 January 2009
DOI: 10.2110/sepmsp.091.099
EISBN: 9781565762961
... 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 turbidites composed of fine-to medium-grained sandstones prevailing over green-gray or dark...
Image
Topological architecture of the multiconnected loop topological prototype i...
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
Journal Article
Journal: AAPG Bulletin
Published: 15 October 2019
AAPG Bulletin (2019) 103 (10): 2369-2398.
... of the reservoir in the field (100–1200 m [330–3900 ft]). The seals are the Verovice and the Lgota shales at the top and bottom of the Grodziszcze and the Lgota sandstones, respectively. The Lgota beds gradually pass upward into the Godula shales and then into the youngest cap rocks that are the Upper Cretaceous...
FIGURES | View All (17)
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985605M843071
EISBN: 9781629810379
... of black shales and radiolarites (Cenomanian) and the Godula beds ( Figure 1 ). Within the northeastern part of the Outer Carpathians, the Godula beds are found regionally and are dominated by clay-rich shales (Godula shales) ( Slaczka et al., 2006 ) that act as cap rocks. These deposits thin to the south...
FIGURES | View All (19)
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985618M843076
EISBN: 9781629810379
... reservoirs (Istebna beds, Ciezkowice Sandstone, and Krosno beds) from the Sile-sian tectonic unit ( Figure 1 ). The outcrop rock samples taken from the Silesian unit were from the Istebna (oldest exposed potential source rocks) and Menilite beds (finely laminated black, organic-rich shales). The outcrop...
FIGURES | View All (11)
Image
Topological architecture and prototypes of multiconnected tree graphoglypti...
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
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985610M843070
EISBN: 9781629810379
... the Lower Cretaceous Spas shales appear at the surface ( Figure 12 ). The synclines are narrow and made up of the Menilite or Krosno beds. Southwest from the town of Przemysl, the folds create a sigmoidal arc that reflects a similar sigmoidal bend of the Carpathian margin. Near the town of Rzeszow...
FIGURES | View All (40)
Journal Article
Published: 01 July 2006
Journal of Foraminiferal Research (2006) 36 (3): 273-275.
... of deep-water agglutinated foraminifera from the hemipelagic variegated shales (Lower Turonian-Lower Santonian) and turbiditic Godula beds (Upper Santonian-Campanian) in the Lanckorona-Wadowice area (Silesian Unit, Outer Carpathians, Poland). p. 259–272, 7 figures. M achaniec , E., G asiniski , M...
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...
FIGURES | View All (7)
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985629M841463
EISBN: 9781629810379
...–grained turbidites and fluxoturbidites (Istebna, Ciezkowice), marls (Weglowka), variegated shales     Late Cretaceous flysch (Ropianka), calcareous turbidites marls, radiolarites, green and red shales thick-bedded, coarse-grained turbidites and fluxoturbidites (Godula, Istebna), flysch (Ropianka...
FIGURES | View All (21)
Journal Article
Published: 01 May 2017
Vadose Zone Journal (2017) 16 (5): 1-9.
... and Sub-Silesian units. The Godula Beds are represented by thin layers of fine-grained sandstones (with glauconite content) and shales. The significance of differences in water properties among the wells in different bedrock types was calculated using the Mann–Whitney U test because the data were...
FIGURES | View All (4)
Series: Geological Society, London, Engineering Geology Special Publications
Published: 01 January 2010
DOI: 10.1144/EGSP23.11
EISBN: 9781862393851
... ; see also Fig.  4 b). The best example of this type of slope deformation occurred on the northern slope of the Ropice Mountain (1082 m) 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...
FIGURES | View All (13)
Series: AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985607M843067
EISBN: 9781629810379
FIGURES | View All (39)
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1979
AAPG Bulletin (1979) 63 (1): 67-86.
... mudstone. B, Thinly bedded, laminated sandstones penetrated by burrows. C, Mollusk burrowing horizontally in mudstone layer. Bar scale = 2 cm. The mudstone is distinctive with a high content of organic matter (organic carbon = 1 to 9%) and pyrite. Also many spherical and flat sideritic...
FIGURES | View All (12)
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...
FIGURES | View All (14)
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP465.24
EISBN: 9781786203656
... and Stryj vicinities. The main goal of these surveys was to map the Miocene anhydrites that form an excellent seismic marker bed within the frontal Carpathians and their foredeep basin (cf. Krzywiec 2001 ). In 1936, ‘Pionier’ purchased another seismic reflection acquisition system, this time from Heiland...
FIGURES | View All (20)
Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.3
EISBN: 9781862393899
... (Schrattenkalk Formation). The latest Cenomanian OAE 2 is represented by the occurrence of black shales in the North Sea (Black Band Bed), the North German Basin (Hesseltal Formation) and numerous Alpine basins of the Eastern Alps and Western Carpathians, as well as by widespread hardground formation...
FIGURES | View All (39)
Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.6
EISBN: 9781862393899
FIGURES | View All (34)