Recurrent Cenozoic volcanic activity in the Bohemian massif (Czech Republic)

J Ulrych, J Dostal, J Adamovič, E Jelínek, P Špaček… - Lithos, 2011 - Elsevier
Cenozoic anorogenic volcanism of the Bohemian Massif is an integral part of the Central
European Volcanic Province. The temporal and spatial distribution of volcanic rocks in the …

A minimum sample size required from Schmidt hammer measurements

T Niedzielski, P Migoń, A Placek - Earth Surface Processes and …, 2009 - Wiley Online Library
The Schmidt hammer is a useful tool applied by geomorphologists to measure rock strength
in field conditions. The essence of field application is to obtain a sufficiently large dataset of …

Constraining long‐term denudation and faulting history in intraplate regions by multisystem thermochronology: An example of the Sudetic Marginal Fault (Bohemian …

M Danišík, P Štěpančíková, NJ Evans - Tectonics, 2012 - Wiley Online Library
The Rychlebské hory Mountain region in the Sudetes (NE Bohemian Massif) provides a
natural laboratory for studies of postorogenic landscape evolution. This work reveals both …

Lithosphere structure of the NE Bohemian Massif (Sudetes)—a teleseismic receiver function study

WH Geissler, H Kämpf, Z Skácelová, J Plomerová… - Tectonophysics, 2012 - Elsevier
In 2004 and 2005 a passive seismic experiment was carried out in the northern and
northeastern part of the Bohemian Massif (Sudetes) to study the lithospheric structure. We …

Damaged speleothems and collapsed karst chambers indicate paleoseismicity of the NE Bohemian Massif (Niedźwiedzia Cave, Poland)

J Szczygieł, A Sobczyk, H Hercman, MJ Mendecki… - …, 2021 - Wiley Online Library
Multiphase speleothem damage and passage collapse in Niedźwiedzia Cave (NE
Bohemian Massif, Poland) were dated with U‐series methods, revealing five events:(1) 320 …

Neotectonic development of drainage networks in the East Sudeten Mountains and monitoring of recent fault displacements (Czech Republic)

P Štěpančíková, J Stemberk, V Vilímek, B Košťák - Geomorphology, 2008 - Elsevier
This paper presents results of morphotectonic research carried out in order to determine the
neotectonic development of the drainage network in the NE spur of the Bohemian Massif …

Meso–Cenozoic cooling and exhumation history of the Orlica‐Śnieżnik Dome (Sudetes, NE Bohemian Massif, Central Europe): Insights from apatite fission‐track …

A Sobczyk, ER Sobel, V Georgieva - Terra Nova, 2020 - Wiley Online Library
This study presents the first suite of apatite fission‐track (AFT) ages from the SE part of the
Western Sudetes. AFT cooling ages from the Orlica‐Śnieżnik Dome and the Upper Nysa …

[PDF][PDF] The Sudetic Marginal Fault: a young morphophotectonic feature at the NE margin of the Bohemian Massif, Central Europe

J Badura, W Zuchiewicz, P Stepancikova… - Acta Geodynamica et …, 2007 - researchgate.net
We analysed a nearly 133-km-long portion of the Sudetic Marginal Fault (SMF) in Poland
(99.7 km) and the Czech Republic (33.8 km), comprised between Złotoryja in the NW and …

[PDF][PDF] The boundary zone of the East and West Sudetes on the 1: 50 000 scale geological map of the Velké Vrbno, Staré Město and Śnieżnik Metamorphic Units

J Don, J Skácel, R Gotowała - Geologia Sudetica, 2003 - researchgate.net
The results of field investigations carried out by the authors were used together with existing
Czech and Polish cartographic publications to compile a digital geological map (1: 50 000) …

Present-day seismicity of the south-eastern Elbe Fault System (NE Bohemian Massif)

P Špaček, Z Sýkorová, J Pazdírková… - Studia geophysica et …, 2006 - Springer
Abstract The Variscan Bohemian Massif is disrupted by the NW-SE striking Elbe Fault
System in its northern part. The increased tectonic activity associated with this structure is …