Geologia
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ISSN 0138-0974
e-ISSN: 2353-0782
Issue Date
2009
Volume
T. 35
Number
Nr 2/1
Description
Journal Volume
Geologia
T. 35 (2009)
Projects
Pages
Articles
Olistolity w serii śląskiej i ich związek z fazami rozwoju basenu śląskiego
(Wydawnictwa AGH, 2009) Cieszkowski, Marek; Golonka, Jan; Krobicki, Michał; Ślączka, Andrzej; Waśkowska, Anna; Wendorff, Marek
Olistoliths of various ages, provenance and dimensions are known in all of the higher-rank tectonic units of the Outer Carpathians. Their occurrences at various stratigraphic levels (Late Jurassic - Early Miocene) are related to different stages of development of the flysch basins, from the stage of rifting to post-rifting, through the orogenic phases, and further to the post-orogenic period.
Rozwój sedymentacji warstw cergowskich jednostki grybowskiej (kamieniołom w Klęczanach, zachodnie Karpaty fliszowe)
(Wydawnictwa AGH, 2009) Stadnik, Renata
The studies were focused on the Cergowa Beds within the northern part of Grybów Unit, the Klęczany-Limanowa tectonic window. The studied formations originated within deep-sea fan, further-more in the quarry there are sediments which belong to middle fan area (subenvironment of channel fill and its margin, interchannel sediments, levee sediments) and outer fan area (despositional lobe).
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.
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.
Refleksyjność witrynitu i typy kerogenu w profilach wierceń wschodniej części Karpat polskich
(Wydawnictwa AGH, 2009) Semyrka, Grażyna
The organic matter in the Krosno formation is represented by type-III kerogen whereas in the Menilite, Inoceramian and Spas shales it ranges from type-II to type-II + III. The vitrinite reflectance values determined for the Krosno and Menilite shales point out that the rocks are immature, while the Inoceramian and Spas shales indicate transformation degree corresponds with the oil window.