In: Geologica Carpathica, vol. 60, no. 4
Anna V. Kalinina - Sergey M. Ammosov - Viktor A. Volkov - Nikolay V. Volkov - Jozef Hok - Ladislav Brimich - Martin Sujan
Detaily:
Rok, strany: 2009, 331 - 338
Jazyk: eng
Kľúčové slová:
Miocene, Western Carpathians, geological structure, microseismic survey, Rayleigh waves, microseisms
URL originálneho zdroja: http://www.geologicacarpathica.com/browse-journal/volumes/60-4/article-488/
O článku:
The microseismic survey method was applied to the study of the geological structures in the region around the Mochovce nuclear power plant. The previous geological and geophysical investigations considered a contact between the Miocene volcanites and sediments as a neotectonic fault. The results of the microseismic investigations allow us to interpret the zone of a supposed neotectonic fault as a transgressive contact of the sediments and the volcanic rocks without a tectonic disruption.
Ako citovať:
ISO 690:
V. Kalinina, A., M. Ammosov, S., A. Volkov, V., V. Volkov, N., Hok, J., Brimich, L., Sujan, M. 2009. Microseismic identification of geological and tectonic structures in the Komjatice Depression (Western Carpathians). In Geologica Carpathica, vol. 60, no.4, pp. 331-338. 1335-0552. DOI: https://doi.org/10.2478/v10096-009-0024-1
APA:
V. Kalinina, A., M. Ammosov, S., A. Volkov, V., V. Volkov, N., Hok, J., Brimich, L., Sujan, M. (2009). Microseismic identification of geological and tectonic structures in the Komjatice Depression (Western Carpathians). Geologica Carpathica, 60(4), 331-338. 1335-0552. DOI: https://doi.org/10.2478/v10096-009-0024-1
O vydaní: