Disentangling polygenetic relief of low mountains at the margin of inland glaciation – Upper Nysa Szalona drainage basin, Sudetes, Central Europe

Author:

Migoń Piotr,Jancewicz KacperORCID,Szymanowski MariuszORCID

Funder

Narodowe Centrum Nauki

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference89 articles.

1. Aleksandrowski, P., Mazur, S., 2002. Collage tectonics in the northeasternmost part of the Variscan belt: the Sudetes, Bohemian Massif. In: Winchester, J.A., Pharaoh, T.C., Verniers, J. (eds), Palaeozoic Amalgamation of Central Europe, Geological Society Special Publication 201, London, pp. 237–277.

2. Badura, J., Przybylski, B., 1998. Zasięgi lądolodów plejstoceńskich i deglacjacja obszaru między Sudetami a Wałem Śląskim [Extent of the Pleistocene ice sheets and deglaciation between the Sudeten Mts. and the Silesian Rampart]. Biuletyn Instytutu Geologicznego 385, 9–28 (in Polish, with Engl. summ.).

3. Badura, J., Przybylski, B., Zuchiewicz, W., 2004, Cainozoic evolution of Lower Silesia, SW Poland: a new interpretation in the light of sub–Cainozoic and sub–Quaternary topography. Acta Geodynamica et Geomaterialia 1(3), 7–29.

4. The Sudetic Marginal Fault: a young morphotectonic feature at the NE margin of the Bohemian Massif, Central Europe;Badura;Acta Geodynamica et Geomaterialia,2007

5. Outline of the geology of the Góry Kaczawskie (Sudetes, Poland);Baranowski;Neues Jahrbuch für Geologie, Paläontologie, Abhandlungen,1990

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