Microseismic identification of geological and tectonic structures in the Komjatice Depression (Western Carpathians)
Published: Aug 2009
Pages: 331 - 338
DOI: https://doi.org/10.2478/v10096-009-0024-1
Authors: ANNA V. KALININA, SERGEY M. AMMOSOV, VIKTOR A. VOLKOV, NIKOLAY V. VOLKOV, JOZEF HOK, LADISLAV BRIMICH, MARTIN SUJAN
Abstract: 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.
Keywords: Miocene, Western Carpathians, geological structure, microseismic survey, Rayleigh waves, microseisms
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