Cadosinopsis rehakovii sp. nov., a new calcareous dinocyst from the Jurassic-Cretaceous transitional interval of the Western Tethys. [PDF]
Variegated limestones, a transitional series between red, Upper Jurassic radiolarite and whitish, Lower Cretaceous Maiolica limestone in the Pieniny Klippen Belt deposits in the Polish part of the Western Carpathians, have yielded rich microfossil ...
Agnieszka Ciurej, Marta Bąk
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Foraminiferal assemblage in the coral-bearing limestones of the Vršatec area (Pieniny Klippen Belt, Western Carpathians, Slovakia) [PDF]
The paper deals with benthic foraminifera occurring with the scleractinian corals in the Jurassic biohermal and peribiohermal coral-bearing limestones of the Vršatec area (Czorsztyn Succession, Slovak Pieniny Klippen Belt).
Morycowa, Elżbieta, Olszewska, Barbara
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Trace fossil curvolithus from the middle Jurassic crinoidal limestones of the Pieniny Klippen Belt (Carpathians, Poland) [PDF]
The trace fossil Curvolithus simplex has been described for the first time in carbonate facies: the Bajocian crinoidal limestones of the Pieniny Klippen Belt. Curvolithus is typical of the Cruziana ichnofacies.
Krobicki, Michał, Uchman, Alfred
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Groundwater impact assessment of Lake Czorsztyn after 25 years of its operation [PDF]
Artificial water reservoirs pose impact on the natural environment. Impact of the artificial Czorsztyn Lake on groundwater and land management is assessed.
Włodzimierz Humnicki +5 more
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Characteristics structures of the mélange zones in the Ukrainian Carpathians
Mélange is characterized by the block-in-matrix fabric in which rigid blocks of different sizes, lithologies, and ages are distributed in a ductile matrix.
O. Hnylko, A. Murovskaya, M. Bohdanova
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Mechanical accumulations of thin Bositra shells form mounds, with complex internal geometries (yellow dots), on the flat top of a drowned carbonate platform, lending an antiformal geometry to their Kimmeridgian–Tithonian drape (above dashed blue line).
Massimo Santantonio, Cristina Muraro
wiley +1 more source
Gravity measurements in the Pieniny Klippen Belt (Western Slovakia) [PDF]
1 Slovak Academy of Sciences, Geophysical Insitute; Dubravska cesta 9, 845 04 Bratislava, Slovakia; e-mail: geofjabu@savba.sk 2 GEOFOS, s.r.o.; Veľký diel 3323, 010 08 Žilina, Slovakia 3 Comenius University, Faculty of Natural Sciences, Department of Applied and Environmental Geophysics; Mlynska dolina, 842 15 Bratislava 4, Slovakia 4 Comenius ...
Jana Bucová +3 more
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Discussion of ‘Olistostromes of the Pieniny Klippen Belt, Northern Carpathians’
J. Golonka, M. Krobicki, A. Waśkowska, M. Cieszkowski & A. Ślączkareply: We welcome the comments by our Slovakian colleagues and their critique of our results, particularly as we have discussed and published papers together several times about our ideas, sometimes, more or less, disputable (Aubrechtet al.2003, 2006; Krobickiet al.2003; Krobicki ...
J. Golonka +5 more
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Geodynamic Studies in the Pieniny Klippen Belt in 2004–2020
ABSTRACT The Pieniny Geodynamic Test Field is situated in the middle of the region between the Inner and Outer Carpathians. Geodynamic research conducted in the past in the Pieniny Klippen Belt (PKB) region were suggestive of neotectonic activity.
Dominika Staniszewska +4 more
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Resolving the Middle Jurassic dinoflagellate radiation: The palynology of the Bajocian of Swabia, southwest Germany [PDF]
Dinoflagellates underwent a major radiation during the Bajocian (Middle Jurassic, ~ 170–168 Ma). The group originated in the Middle Triassic and dinoflagellate cysts were relatively low in diversity until the Bajocian, when over 100 species appeared. The
Franz, M, Riding, JB, Wiggan, NJ
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