National Repository of Grey Literature 3 records found  Search took 0.01 seconds. 
Dukovany nuclear power station. Seismotectonic model. Geological and paleoseismic survey. Sectio A – Assesment of the Diendorf-Boskovice fault zone
Špaček, P. ; Roštínský, Pavel ; Prachař, I. ; Švancara, J. ; Valenta, J. ; Tábořík, P.
Synthesis of geological (structural, tectonic, sedimentological), geophysical (gravimetric, geomagnetic) and geomorphological (topographic arrangement, surface inclination, topolineaments, fluvial system, segmentation of the area along the fault) knowledge on the major fault of the Diendorf-Boskovice tectonic zone. Existing data were completed with a new direct field research (ground geophysics – ERT, borehole survey, study of outcrops and geomorphological conditions along the major fault). The study was elaborated requested by ČEZ corporation (main Czech energetic producer) in connection with the assessment of seismic hazard to the near Dukovany nuclear power station related both to a renewal of working license of existing facilities (two production units) and to a planned extension of energetic system by a third production installation. It was especially focused on the nearest fault section Tetčice – Hostěradice in the Czech Republic. In the closing section, a rate of potential Upper Quaternary tectonic activity related to evidenced geotectonically active period of Lower Miocene were evaluated. The report will serve as a basic source for a compilation of seismic model of the Diendorf-Boskovice zone.
Sedimentary covers in the Bohutický les Upland area and their relation to the topography evolution
Roštínský, Pavel
The paper presents basic notes on geology and geomorphology of the Bohutický les Upland (South Moravia), an asymmetric horst situated in the contact area between the Bohemian Massif and Carpathian Foredeep. The distinct western scarp and some other striking morphological features of the elevation originated through the multi-phase alpine neotectonic transtensile reactivation of the important Diendorf Fault and associated dislocations in the Neogene and Quaternary. A complicated mosaic of solid Proterozoic/Palaeozoic bed-rocks, poorly consolidated Neogene clastics and Quaternary sediments developed in the area.
Tectonic style of the SE margin of the Bohemian Massif in southern Moravia and northern Austria
Roštínský, Pavel
The contribution deals with geotectonic position, tectonic configuration and general geomorphology of the south-western section of the marginal part of the Bohemian Massif. The 100 km long marginal flank is formed by the regionally important linear Diendorf fault system of Paleozoic age. During Cenozoic, this old tectonic area was reactivated in transtensile regime as a one of zones compensating different movements between the Eastern Alps and Western Carpathians. Thus, from a kinematic point of view, it can be regarded as a component of the Alpine orogen.

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