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Ostrava Formation

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FIGURE 3 —Generalized stratigraphy of the <span class="search-highlight">Ostrava</span> <span class="search-highlight">Formation</span>, goniatite zone...
Published: 01 June 2009
FIGURE 3 —Generalized stratigraphy of the Ostrava Formation, goniatite zones, and the major, basinwide marine zones (IV, Leonard; IX, Naneta; XII, Františka; XVI, Enna; XVII, Šusta; XXI, Barbora; and XXVII, Gaebler) within and separating members. The Pendleian and Arnsbergian are substages
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FIGURE 7 —Dendrogram plot of the <span class="search-highlight">Ostrava</span> <span class="search-highlight">Formation</span> macrofloral assemblages ...
Published: 01 June 2009
FIGURE 7 —Dendrogram plot of the Ostrava Formation macrofloral assemblages in named genetic cycles following constrained cluster analysis using unweighted pair group method with arithmetic mean in MVSP, ver. 3.1 ( Kovach, 2006 ). The results of the four- and five-class solutions using Bayesian
Journal Article
Journal: PALAIOS
Published: 01 June 2009
PALAIOS (2009) 24 (6): 336–350.
...FIGURE 3 —Generalized stratigraphy of the Ostrava Formation, goniatite zones, and the major, basinwide marine zones (IV, Leonard; IX, Naneta; XII, Františka; XVI, Enna; XVII, Šusta; XXI, Barbora; and XXVII, Gaebler) within and separating members. The Pendleian and Arnsbergian are substages...
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Series: Geological Society, London, Special Publications
Published: 21 July 2023
DOI: 10.1144/SP524-2021-118
EISBN: 9781786209566
... exemplified by the separation of South America from Africa. This inherited origin has been used in any model of formation where the continental separation line follows a step-like configuration, alternating transform and divergent segments (e.g. among many others Le Pichon and Hayes 1971 ; Scrutton 1979...
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Series: Geological Society, London, Special Publications
Published: 21 July 2023
DOI: 10.1144/SP524-2021-96
EISBN: 9781786209566
... domains, and finally, (3) throws light on the formation of TMPs. We analyse two existing wide-angle seismic-derived velocity models from the MARGATS seismic experiment (Demerara Plateau), and adjacent composite industrial seismic lines covering the Demerara and Guinea plateaus. The Demerara Plateau...
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FIGURE 3 —Biostratigraphic ranges of  Lyginopteris  species (left; first us...
Published: 01 June 2009
FIGURE 3 —Biostratigraphic ranges of Lyginopteris species (left; first used by Patteisky, 1937 , 1957 ), megafloral zones (center; Purkyňová, 1977 , 1996b ), and cluster analysis of megafloral taxa (right; Gastaldo et al., 2009 ) in the Ostrava Formation. Four classes of plant-fossil
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FIGURE 2 —Map of the <span class="search-highlight">Ostrava</span>-Karvina coalfield. A) Mining districts from wh...
Published: 01 June 2009
FIGURE 2 —Map of the Ostrava-Karvina coalfield. A) Mining districts from which borehole data were acquired are outlined; the W–E line depicts the basinal cross section shown in B. B) Distribution and thickness of coal-bearing members of the Mississippian Ostrava Formation in stratigraphic order
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FIGURE 1 —Geographic and geologic features of the Upper Silesian Basin. A) ...
Published: 01 June 2009
Block. C) Geographic distribution of only the Paleozoic rocks, including the members of the Ostrava Formation, in the Silesian Basin (after Dopita et al., 1997 ). Mesozoic and Cenozoic overburden, which may attain 2000 m in thickness in the southeast, has been removed from the illustration
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TABLE 1 —Last appearance (LAD) and first appearance data (FAD) for megaflor...
Published: 01 June 2009
TABLE 1 —Last appearance (LAD) and first appearance data (FAD) for megafloral elements across the Enna Marine Zone, marking the change from the Hrušov to Jaklovec Members of the Ostrava Formation. Present data set supplemented by Purkyňová (1996a, 1996b)
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TABLE 2 —Last appearance (LAD) and first appearance data (FAD) for megaflor...
Published: 01 June 2009
TABLE 2 —Last appearance (LAD) and first appearance data (FAD) for megafloral elements across the Barbora Marine Zone, marking the change from the Jaklovec to Poruba Members of the Ostrava Formation. Present data set supplemented by Purkyňová (1977, 1996a, 1996b)
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FIGURE 2 —Stratigraphic relationships in the Upper Mississippian <span class="search-highlight">Ostrava</span> Fo...
Published: 01 June 2009
FIGURE 2 —Stratigraphic relationships in the Upper Mississippian Ostrava Formation, which is subdivided into four members: Petřkovice, Hrušov, Jaklovec, and Poruba. Each member is separated by a basin-wide, thick marine interval identified by roman numerals (as established by Řehoř
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Stratigraphy and facies distribution within the southern (southern Moravia,...
Published: 01 January 2001
Fig. 3. Stratigraphy and facies distribution within the southern (southern Moravia, Drahany) and northern parts (northern Moravia and Silesia, Nízký Jeseník) of the basin. OF, Ostrava Formation; HKF, Hradec–Kyjovice Formation; MF, Moravice Formation; HBF, Horní Benešov Formation; AHF
Journal Article
Journal: PALAIOS
Published: 01 June 2009
PALAIOS (2009) 24 (6): 351–366.
...FIGURE 3 —Biostratigraphic ranges of Lyginopteris species (left; first used by Patteisky, 1937 , 1957 ), megafloral zones (center; Purkyňová, 1977 , 1996b ), and cluster analysis of megafloral taxa (right; Gastaldo et al., 2009 ) in the Ostrava Formation. Four classes of plant-fossil...
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Journal Article
Published: 01 October 2014
Mineralogical Magazine (2014) 78 (5): 1265–1286.
... to marine facies and there are frequent intercalations of a volcanoclastic material. This type of sedimentation is characterized by the cyclic alternation of clastic sediments with coal beds. The formation called the Ostrava Formation (Paralic Series in Poland) consists of the Petřkovice, Hrušov, Jaklovec...
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Journal Article
Published: 25 January 2017
Quarterly Journal of Engineering Geology and Hydrogeology (2017) 50 (1): 53–59.
... become a geotourism post-mining landmark associated with black coal mining in Ostrava, the third largest city in the Czech Republic. At the same time, Ostrava is the largest industrial city in the Czech Republic. The study analyses a new approach to assess the surface area thermal activity in coal...
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Journal Article
Published: 01 March 2008
Journal of Environmental and Engineering Geophysics (2008) 13 (1): 13–26.
...Dalibor Matysek; Helena Raclavska; Konstantin Raclavsky Abstract Magnetic susceptibility measurements were performed on 2,000 samples of forest soils from the Ostrava-Karvina industrial region (Czech part of Upper Silesian Coal Basin) and the Moravian-Silesian Beskydy Mountains and their piedmont...
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Journal Article
Published: 01 May 2012
Quarterly Journal of Engineering Geology and Hydrogeology (2012) 45 (2): 231–241.
... 25 km NE of Ostrava and its establishment merged the former CSA (Czechoslovak Army) and Lazy Mines on 1 April 2008. The seam thickness of the Karvina Formation reaches c . 1.5–5 m; the basal seam of the formation is generally almost connected with the overlying seam and reaches 10 m thickness...
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TABLE 1 —Genetic cycles identified in the <span class="search-highlight">Ostrava</span> and lowermost Karvina For...
Published: 01 June 2009
TABLE 1 —Genetic cycles identified in the Ostrava and lowermost Karvina Formations, Upper Silesian Basin, Czech Republic, based on a composite section. Cycles are placed within members of each formation according to Dopita and Kumpera (1993). Groups identified using unweighted pair group method
Journal Article
Published: 01 December 2021
American Mineralogist (2021) 106 (12): 2028–2030.
..., the next year Peacock showed that goldschmidtine was in fact stephanite. The new goldschmidtite mineral was found as an inclusion in a diamond from the Kaapavaal craton in South Africa. From single-clinopyroxene geothermobarometry, the authors estimate that the pressure-temperature of formation was 53...
Journal Article
Published: 01 January 2001
Journal of the Geological Society (2001) 158 (1): 137–150.
...Fig. 3. Stratigraphy and facies distribution within the southern (southern Moravia, Drahany) and northern parts (northern Moravia and Silesia, Nízký Jeseník) of the basin. OF, Ostrava Formation; HKF, Hradec–Kyjovice Formation; MF, Moravice Formation; HBF, Horní Benešov Formation; AHF...
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