An olistolith interpretation for the Paleocene Szydłowiec sandstones in the stratotype area (Outer Carpathians, Poland) [PDF]
, 2012 The thick-bedded complex of the Szydłowiec sandstones belongs to the lithological succession of the Subsilesian sedimentary area in the Polish Outer Carpathians.
Cieszkowski, Marek +2 more
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Annales Societatis Geologorum Poloniae, 2015 The calcareous nannoplankton and foraminifera from the Gladyszow Beds, regarded as the youngest deposits in the northern marginal Siary Subunit of the Magura Nappe in Poland, are characterized. The material investigated comes from outcrops in the vicinity of Gladyszow and from the Gladyszow PIG-1 borehole.
Małgorzata Garecka, Andrzej Szydło
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Geologica Carpathica, 2010 The lithostratigraphy and biostratigraphy of the Bystrica/Tylicz and Krynica facies zones of the Magura Nappe have been studied in the Beskid Sadecki Range and Lubovnianska Vrchovina (Polish and Slovak parts of the Western Outer Carpathians respectively).
Oszczypko, Nestor +1 more
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Digital Elevation Model (DEM) applied to geological research : a case study of the area between Dobczyce and Mszana Dolna (Polish Outer Carpathians, southern Poland [PDF]
, 2004 This paper is a preliminary report on using the Digital Elevation Model (DEM) and Shaded Relief Image in geological mapping in the Carpathians. Digital processing of the topographical maps in 1:25 000 scale enabled 3D visualization of a fragment of olish
Chodyń, Rafał
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Remarks on the type locality and current status of the foraminiferal species Rzehakina epigona (Rzehak, 1895) [PDF]
, 2001 A likely topotype locality is proposed for Rzehakina epigona. As the type specimen of Silicina epigona Rzehak, 1895 is assumed to be lost, we undertook a search for new material in the type area, Zdounky village in Moravia. A single locality provided a
Bubik, M., Kaminski, M.A.
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The application of morphostructural analysis and its validation by comparison with documented faults within the Zlate Hory ore district (the Northeastern part of the Bohemian Massif) [PDF]
, 2013 The goal of this study is to determine the validity of morpholineaments network that was inferred based on morphostructural analysis of digital elevation model (DEM), by crosschecking with documented faults.
Daněk, Tomáš +4 more
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Foraminifera from the Eocene variegated shales near Barwinek (Magura unit, Outer Carpathians), the type locality of Noth (1912) revisited [PDF]
, 2017 This is the final version of the article. Available from the Polish Geological Society via the URL in this record.A rich deep-water agglutinated foraminifera (DWAF) fauna (approximately 50 taxa) is documented from the lower to middle Eocene Variegated ...
Cieszkowski, M, Kaminski, MA, Kender, S
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Where was the Magura Ocean? [PDF]
, 2015 In the Late Jurassic to Early Cretaceous palaeogeography of the Alpine Tethys the term Ocean is used for different parts of these sedimentary areas: eg. Ligurian-Piedmont and Penninic, Magura, Pieniny, Valais and Ceahlau-Severins oceans. The Magura Ocean
Olszewska, Barbara +3 more
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The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units [PDF]
, 2018 A correlation of tectonic units of the Alpine-Carpathian-Dinaridic system of orogens, including the substrate of the Pannonian and Transylvanian basins, is presented in the form of a map.
Bernoulli, Daniel +7 more
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Geodynamics and paleogeography of the Silesian Ridge in the Outer Carpathians [PDF]
, 2014 The complex Mesozoic and Cenozoic tectonics of the Outer Carpathians produced series of ridges separating deep water basins.The Silesian Ridge existed since from Jurassic till Oligocene times.
Cieszkowski, Marek +4 more
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