Facebook Instagram Twitter RSS Feed PodBean Back to top on side

Physical properties of Hradište border fault (Turiec Basin, Western Carpathians, Slovakia) inferred by multidisciplinary geophysical approach

In: Geologica Carpathica, vol. 71, no. 1
David Kušnirák - Hermann Zeyen - Miroslav Bielik Číslo ORCID - René Putiška - Andrej Mojzeš Číslo ORCID - Bibiana Brixová - Roman Pašteka - Ivan Dostál - Pavol Zahorec - Juraj Papčo Číslo ORCID - Jozef Hók - Marián Bošanský - Martin Krajňák

Details:

Year, pages: 2020, 3 - 13
Language: eng
Keywords:
Near-surface geophysics, seismic tomography, electrical resistivity tomography, ground-penetrating radar, self-potential, radiometry, gravimetry, magnetometry, border fault, Turiec Basin, Western Carpathians
About article:
The Hradište border fault zone has played an important role in the development of the tectonic contact of the Cenozoic sediments of the Turiec Basin with the Malá Fatra Mountains crystalline basement. Seismic, geoelectric, radiometric, gravimetric, magnetometric and ground penetrating radar measurements were used to study the physical properties and determine the exact position and inclination of this fault zone down to a depth of up to 40 m. The Hradište border fault zone represents an almost vertical physical boundary characterized by decreasing seismic velocity (from 3.0 km.s−1 to 2.2 km.s−1) and decreasing electrical resistivity (500 to 150 Ω.m) when passing from the basement west of the fault to sediments to its east. It corresponds also to a compact segment of the lowest volume activity of radon 222Rn values in soil air (8 kBq.m−3 on average) and maximum horizontal gravity gradient (−0.0076 mGal.m−1). The discovery of this anomalous zone also helps us to distinguish two different anomalous blocks. The block west of the fault represents the orthogneisses of the Tatric crystalline complex belonging to the Malá Fatra Mountains. The eastern block is built-up by the Bystrička Member Pliocene sediments of the Turiec Basin. Our study serves as a case study for geophysical research on faults in different tectonic units of the Western Carpathians and other similar orogens.
How to cite:
ISO 690:
Kušnirák, D., Zeyen, H., Bielik, M., Putiška, R., Mojzeš, A., Brixová, B., Pašteka, R., Dostál, I., Zahorec, P., Papčo, J., Hók, J., Bošanský, M., Krajňák, M. 2020. Physical properties of Hradište border fault (Turiec Basin, Western Carpathians, Slovakia) inferred by multidisciplinary geophysical approach. In Geologica Carpathica, vol. 71, no.1, pp. 3-13. 1335-0552. DOI: https://doi.org/10.31577/GeolCarp.71.1.1

APA:
Kušnirák, D., Zeyen, H., Bielik, M., Putiška, R., Mojzeš, A., Brixová, B., Pašteka, R., Dostál, I., Zahorec, P., Papčo, J., Hók, J., Bošanský, M., Krajňák, M. (2020). Physical properties of Hradište border fault (Turiec Basin, Western Carpathians, Slovakia) inferred by multidisciplinary geophysical approach. Geologica Carpathica, 71(1), 3-13. 1335-0552. DOI: https://doi.org/10.31577/GeolCarp.71.1.1
About edition:
Published: 17. 2. 2020