Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Otília Lintnerová"'
Publikováno v:
Geologica Carpathica, Vol 68, Iss 5, Pp 385-402 (2017)
The production of platform carbonates of the Manín Unit (Manín Straits, Central Western Carpathians) belonging to the Podhorie and Manín formations and formed by remains of rudists and benthic foraminifers (Urgonian-type carbonates), was previousl
Publikováno v:
Geological Quarterly.
Tectonic setting of both the uppermost Triassic Tomanova and the lowermost Jurassic Dudziniec formations can be characterized by a series of diagnostic discrimination diagrams. High-silica and low-silica multi-dimensional diagrams indicate that the s
Autor:
Jozef Michalík, Daniela Reháková, Jacek Grabowski, Otília Lintnerová, Petr Schnabl, Šimon Kdýr
Publikováno v:
Cretaceous Research. 118:104659
An integrated study of micro- and nannoplankton distribution, O and C isotopes and palaeomagnetic record of nine Carpathian sections provided a key interpretation tool to characterize the Jurassic–Cretaceous (J/K) boundary transition. Biostratigrap
Publikováno v:
Volumina Jurassica.
The Jurassic / Lower Cretaceous sequence of the Strážovce section has been deposited in the central, axial part of the Zliechov Basin. Its most characteristic part – the Ždiar Formation consists of bedded siliceous radiolarian limestones and rad
Autor:
Jacek Grabowski, Otília Lintnerová, Marián Golej, Vladimír Šimo, Barbara Zahradníková, Andrzej Gaździcki, Patrycja Wójcik-Tabol, Jozef Michalík
Publikováno v:
Geologica Carpathica. 64:39-62
Terminal Triassic environmental changes are characterized by an integrated study of lithology, litho- and cyclostratigraphy, paleontology, mineralogy, geochemistry and rock magnetism in the Tatra Mts. The Carpathian Keuper sequence was deposited in a
Publikováno v:
Cretaceous Research. 38:68-79
The base of Lower Cretaceous sequence in the Manin Unit is erosive but without signs of subaerial emersion. Submarine erosion was triggered by bottom denivelization during Late Berriasian extension of the area. Sedimentation of planktogenic hemipelag
Publikováno v:
Geologica Carpathica. 61:309-326
Magneto-, and isotope stratigraphy around the Jurassic/Cretaceous boundary in the Vysoká Unit (Malé Karpaty Mountains, Slovakia): correlations and tectonic implications Magneto- and isotope stratigraphic studies in the Vysoká Nappe (Hlboča sectio
Publikováno v:
Geologica Carpathica. 60:213-232
The Brodno section — a potential regional stratotype of the Jurassic/Cretaceous boundary (Western Carpathians) Compared to coeval successions from the Carpathians, the continuous Jurassic-Cretaceous (J/K) pelagic limestone succession of the Brodno
Autor:
Otília Lintnerová, Petr Skupien, Jozef Michalík, Marta Bąk, Eva Halásová, Daniela Boorová, Ján Soták
Publikováno v:
Cretaceous Research. 29:871-892
During the Jurassic and Cretaceous, the Pieniny Klippen Belt units of the Outer Western Carpathians were situated on the edge of the Paleoeuropean shelf rimming the northermost margin of the Mediterranean Tethys. During the late early Aptian humid ev
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 244:71-88
The Fatra and Kopieniec formations in the Zliechov Basin comprise a record of several environmental crises that may have contributed to the global Triassic–Jurassic (T–J) boundary events. The diversity of the benthic fauna decreases at the base o