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Czorsztyn Unit

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- Geographic locations of ten sections (belonging to the <b>Czorsztyn</b> <b>Unit</b>) in...
Published: 01 February 2020
Fig. 1 - Geographic locations of ten sections (belonging to the Czorsztyn Unit) in the Pieniny Klippen Belt and two sections belonging to the Peri-klippen units (Butkov in the Manín Unit and Podbranč in the Drietoma Unit), coded according to their environmental affinity during the Middle Jurassic
Journal Article
Published: 01 March 2008
Journal of Paleontology (2008) 82 (2): 351–361.
...Ján Schlögl; Jozef Michalík; Kamil Zágoršek; François Atrops Abstract A Lower Tithonian cavity-dwelling community from pelagic carbonate platform deposits of the Czorsztyn Unit, Western Carpathians, represents a succession of mostly solitary coelobite organisms, dominated by scleractinian...
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Journal Article
Published: 25 July 2014
Geological Magazine (2015) 152 (2): 269–286.
... the less-competent rocks (mainly flysch, shales and marls). The Niedzica Unit (southeast of Czorsztyn Succession in the Pieniny Basin; Golonka & Krobicki, 2004 ; Wierzbowski et al. 2004 ) is located next to the thick Czorsztyn Unit (Birkenmajer, 1970...
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Journal Article
Published: 01 January 2009
Bulletin de la Société Géologique de France (2009) 180 (1): 27–38.
...-walled taxa recorded. This is surprising in that the same deeper-water areas still existed in the western Tethys. In the Czorsztyn Limestone Formation [ Birkenmajer, 1963 , 1977 , 1986 ; Hudson et al ., 2005 ] of southern Poland, the limestones of the Pieniny Klippen Belt [ Lewandowski et al...
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Journal Article
Published: 01 December 2007
Journal of Sedimentary Research (2007) 77 (12): 1026–1045.
.... 1999 ), the Jurassic Oolithe Ferrugineuse de Bayeux (northern France; Preat et al. 2000 ) and the Czorsztyn Unit (Slovakia; Jurassic; Aubrecht et al. 2002 ). Red carbonates in proximal ramp environments include the Krupianka Formation (Slovakia; Jurassic; Aubrecht et al. 2002 ; Aubrecht and Szulc...
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985620M843078
EISBN: 9781629810379
... of lithosphere fragments from the Alpine realm, as well as the rise of the Pannonian asthenolite. The Paleozoic units of the Inner Western Carpathians have their hydrocarbon potential practically exhausted. The oldest Paleozoic units of the Tatricum, Veporicum, and Gemericum are altered by different grades...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.6
EISBN: 9781862393899
..., continental margins, and continental fragments. The Western Alps form a pronounced, westward-convex arc around which the strike of the tectonic units changes by almost 180° ( Fig. 18.1 ). The Western Carpathians are a northward-convex arc of similar size but with minor curvature. The two arcs are connected...
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Journal Article
Published: 01 February 2020
Italian Journal of Geosciences (2020) 139 (1): 76–97.
...Fig. 1 - Geographic locations of ten sections (belonging to the Czorsztyn Unit) in the Pieniny Klippen Belt and two sections belonging to the Peri-klippen units (Butkov in the Manín Unit and Podbranč in the Drietoma Unit), coded according to their environmental affinity during the Middle Jurassic...
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Journal Article
Published: 01 January 2017
Geological Magazine (2017) 154 (1): 193–200.
... that ‘there are many still unresolved problems in the geology of the PKB’. We also agree with the statement ‘olistostromes and olistoliths are quite frequent, but not omnipresent’. We depicted the distribution of the olistoliths and their relationship to the non-olistolith tectonic units of the PKB in Golonka et al...
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/985606M843066
EISBN: 9781629810379
...–Aalenian had to precede the appearance of the Czorsztyn ridge, which did not exist as the main paleogeographic unit before Bajocian (e.g., Aubrecht et al., 1997 ). This ridge emergence was connected with the postrift phase of the basin evolution ( Golonka and Slaczka, 2003 ). The sedimentation...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP425.1
EISBN: 9781862399570
... (North. Gemericum) 48.8, 20.1 Carnian 2/8 308 44 – – 314 55 – – −46±?? 54 286 – – ** 15 Bódva nappe 41 Rudabánya Mountains T2 5 33 72 5 41 298 43 20 17 −62±23 37 288 13 21 f+ 14 Pieniny Klippen Belt 42 Czorsztyn unit–Primary...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.2
EISBN: 9781862393899
... of which seven are used today (although none of them has retained its original strati graphic range). Albert Oppel (1856-1858) developed a sequence of such divisions for the entire Jurassic System, crucially using the units in the sense of time divisions. Abstract The Jurassic System (199.6-145.5 Ma...
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Series: GSA Memoirs
Published: 01 January 2007
DOI: 10.1130/2007.1200(17)
... zone, the crust is ∼40 km thick, but most of its upper half is the sedimentary fill of the late Paleozoic and Mesozoic Polish trough, which is underlain by a thick sequence of older continental-margin volcanic and sedimentary units. The lithospheric mantle structure is complex and indicative of a plate...
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Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2009
DOI: 10.2110/sepmsp.091.013
EISBN: 9781565762961
... using the end members clay, carbonate, and chert: deep-water red claystones deposited below the calcite compensation depth, red hemipelagic and pelagic carbonates, and red cherts and radiolarites. The depositional environment of most CORB units was in relatively deep oceanic basins. Deposition...
Journal Article
Published: 26 November 2020
Journal of the Geological Society (2021) 178 (2): jgs2020-021.
... . Stratigraphy and palaeogeography of the Czorsztyn series (Pieniny Klippen Belt, Carpathians) Poland . Studia Geologica Polonica , 9 , 380 [in Polish, with English summary] . Birkenmajer , K. 1977 . Jurassic and Cretaceous lithostratigraphic units of the Pieniny Klippen Belt, Carpathians, Poland...
Journal Article
Published: 23 October 2019
Journal of the Geological Society (2020) 177 (3): 629–646.
... was distinguished by Birkenmajer (1986) as the Klippen Belt Basin and by Plašienka (2018) as the Vahic unit. According to ( Golonka et al. 2017 ) the Jurassic–Lower Cretaceous rocks deposited on the northwestern slopes belong to the Czorsztyn, Niedzica, Czertezik, Branisko and Pieniny PKB klippen successions...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2003
DOI: 10.1144/GSL.SP.2003.208.01.07
EISBN: 9781862394568
... limestones) of the Złatna Unit ( Sikora 1971 ; Golonka & Sikora 1981 ) later also described as the Ultrapieninic unit or Vahicum (e.g. Birkenmajer 1986 ; Plašienka 1999 ). The transitional slope sequences between deepest basinal units and ridge units (Czorsztyn Ridge – Fig. 6 – CR) are known...
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Journal Article
Published: 01 July 2012
Journal of Micropalaeontology (2012) 31 (2): 97–109.
..., sediments are often unfossiliferous red clays ( Hu et al ., 2005 ) devoid of planktic foraminifera. In the Czorsztyn Limestone Formation ( Birkenmajer, 1977 ; Hudson et al ., 2005 ) of southern Poland, the limestones of the Pieniny Klippen Belt ( Birkenmajer, 1963 , 1977 , 1986 ; Krobicki &...
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Journal Article
Published: 03 March 2021
Seismological Research Letters (2021) 92 (3): 1717–1725.
... in connection with the artificial Czorsztyn Lake’s impoundment for hydropower plant purposes ( Białoń et al. , 2015 ) and with hydrofracturing in shale gas pilot projects ( López‐Comino et al. , 2018 ). Although the natural seismicity in Poland is not hazardous, the mining‐induced earthquakes often cause...
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Journal Article
Published: 26 November 2020
Journal of the Geological Society (2021) 178 (2): jgs2020-111.
... of the Złatne Unit, as well as the relationship between the PKB, Central and Outer Carpathians. Sikora (1971) introduced the Złatne Succession and the Złatne Basin, which were redefined by Golonka and Krobicki (2004) , using the modern paleogeographic approach. This basin was part of the Alpine Tethys, which...
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