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Browsing by Author "Skupien, Petr"

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  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Dolomitization in diagenetic history of the Štramberk limestones
    (Wydawnictwa AGH, 2008) Lintnerová, Otília; Knietl, Marian; Reháková, Daniela; Skupien, Petr; Vašíček, Zdenĕk
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    Item type:Article, Access status: Open Access ,
    Główne elementy paleogeograficzne Zachodnich Karpat zewnętrznych w późnej jurze i wczesnej kredzie
    (Wydawnictwa AGH, 2008) Golonka, Jan; Krobicki, Michał; Waśkowska, Anna; Vašíček, Zdenĕk; Skupien, Petr
    The present paper concentrates on the elements important to understanding the paleogeography of the West Carpathians during Late Jurassic and Early Cretaceous times. These elements are linked to the lithostratigraphy of the various facies zones as well as occurrence of hydrocarbon source rocks. Several paleogeographic elements have been described: the Alpine Tethys, Magura Basin, Silesian Ridge, Severin-Moldavidic Basin and North European Platform. The uplifted and basinal zones were distinguished within the platform. The Baska-Inwałd Ridge and Pavlov Carbonate Platform belong to the uplifted elements, while Bachowice and Mikulov basins represent the basinal zones.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Górnojurajsko-dolnokredowe skały macierzyste w zachodniej części Karpat fliszowych
    (Wydawnictwa AGH, 2008) Golonka, Jan; Matyasik, Irena; Skupien, Petr; Więcław, Dariusz; Waśkowska, Anna; Krobicki, Michał; Strzeboński, Piotr Andrzej; Vašíček, Zdenĕk
    The analysis of possibility to find Upper Jurassic-Lower Cretaceous source rocks in the western part of Flysch Carpathians in Poland and Czech Republic was the subject of present paper. The Upper Jurassic organic-rich Mikulov marls represent world-class source rocks. These 1400 m thick organic-rich rocks with TOC value 0.2 $\div$ 10% sourced oils in the Vienna Basin and Carpathian subthrust in Czech Republic and Austria. The similar source rocks perhaps exist in the deeper subthrust areas in Poland. The Vendryne Formation rocks do not contain significant amount of organic carbon. The increased TOC was encountered within the Verovice Formation and uppermost part of Hradiste Formatio. These rocks represent global anoxic event OAE 1b. Verovice Formation contains potential source rocks for the Outer Carpathians systems with reservoirs various in age.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Litostratygrafia osadów górnej jury i dolnej kredy zachodniej części Karpat zewnętrznych (propozycja do dyskusji)
    (Wydawnictwa AGH, 2008) Golonka, Jan; Vašíček, Zdenĕk; Skupien, Petr; Waśkowska, Anna; Krobicki, Michał; Cieszkowski, Marek; Ślączka, Andrzej; Słomka, Tadeusz
    Upper Jurassic-Lower Cretaceous deposits are part of the Outer Carpathians nappes: Magura, Silesian and Sub-Silesian-Żdanice-Waschberg, and are known in olistholites, which occur within different units of the Outer Carpathians. Authors systematized lithostratigraphical units according to their primary position in sedimentary basins and other sedimentary areas. Magura Basin originated in Middle Jurassic and proto-Silesian Basin in Late Jurassic-Early Cretaceous times together with syn- and post-rift deposits. Sub-Silesian-Żdanice sedimentary area originated in Late Cretaceous, and during Jurassic and Early Cretaceous times was northern part of the proto-Silesian Basin. The source areas for olistholites have been northern slope and shelf of the proto-Silesian Basin and submerged intra-oceanic ridges (cordilleras).
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    Item type:Article, Access status: Open Access ,
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Utwory formacji wierzowskiej na tle wczesnokredowych warunków sedymentacji w zachodniej części basenu protośląskiego (Morawy, Republika Czeska)
    (Wydawnictwa AGH, 2009) Strzeboński, Piotr Andrzej; Golonka, Jan; Waśkowska, Anna; Krobicki, Michał; Słomka, Tadeusz; Skupien, Petr; Vašíček, Zdenĕk
    Sedimentological development of the Verovice Formation (Czech Moravia) is presented, according to Early Cretaceous geotectonic-eustatic changes in the proto-Silesian Basin. Those processes were a consequence of a gradual rebuilding the architecture of the Alpine-Carpathian realm. The geological events well correspond with the global sequence stratigraphy.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Utwory wczesnokredowego basenu protośląskiego w polsko-czeskich Karpatach fliszowych
    (Wydawnictwa AGH, 2009) Waśkowska, Anna; Golonka, Jan; Strzeboński, Piotr Andrzej; Krobicki, Michał; Vašíček, Zdenĕk; Skupien, Petr
    The proto-Silesian Basin was well developed within the Alpine Tethys during the Late Jurassic times and existed as undivided entity until the significant Late Cretaceous reorganization. The deposits originated within this basin were incorporated into different structural units: Silesian, Subsilesian and Skole. The calciturbiditic Cieszyn Limestone Formation is the oldest Cretaceous flischoidal sequence of the proto-Silesian Basin. This calciturbiditic sedimentation passed gradually into younger siliciclastic deposition.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Western Carpathians in the territory of the Czech Republic
    (Wydawnictwa AGH, 2008) Skupien, Petr; Vašíček, Zdenĕk