Damaged Speleothems and Collapsed Karst Chambers Indicate Paleoseismicity of the NE Bohemian Massif (Niedźwiedzia Cave, Poland)
Author:
Affiliation:
1. Institute of Earth Sciences University of Silesia Sosnowiec Poland
2. Institute of Geological Sciences University of Wrocław Wrocław Poland
3. Institute of Geological Sciences Polish Academy of Sciences Warszawa Poland
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020TC006459
Reference97 articles.
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3. Pleistocene speleothem fracturing in the foreland of the Western Carpathians: A case study from the seismically active eastern margin of the Bohemian Massif;Bábek O.;Geological Quarterly,2015
4. Ancient DNA and dating of cave bear remains from Niedźwiedzia Cave suggest early appearance of Ursus ingressus in Sudetes
5. Extent of the Pleistocene ice sheets and deglaciation between the Sudeten and the Silesian Rampart;Badura J.;Biuletyn Państwowego Instytutu Geologicznego,1998
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