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Present-day stress orientation and tectonic pulses registered in the caves of the Slovenský kras Mts. (South-Eastern Slovakia)
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SYSNO ASEP 0496087 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Present-day stress orientation and tectonic pulses registered in the caves of the Slovenský kras Mts. (South-Eastern Slovakia) Author(s) Briestenský, Miloš (USMH-B) RID, ORCID
Hochmuth, Z. (SK)
Littva, J. (SK)
Hók, J. (SK)
Dobrovič, R. (SK)
Stemberk, Josef (USMH-B) RID, ORCID
Petro, L. (SK)
Bella, P. (SK)Source Title Acta geodynamica et geomaterialia. - : Ústav struktury a mechaniky hornin AV ČR, v. v. i. - ISSN 1214-9705
Roč. 15, č. 2 (2018), s. 93-103Number of pages 11 s. Publication form Print - P Language eng - English Country CZ - Czech Republic Keywords Neotectonics ; Microdisplacement monitoring ; Cavitonics ; Recent geodynamics Subject RIV DB - Geology ; Mineralogy OECD category Geology R&D Projects LM2015079 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) OC 625.10 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) LM2010008 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) Institutional support USMH-B - RVO:67985891 UT WOS 000437412800001 DOI 10.13168/AGG.2018.0007 Annotation The fault displacement monitoring network EU-TecNet was established to define microdisplacements across faults in the territory of Central Europe (www.tecnet.ez) using three-dimensional optical-mechanical extensometers. The results of long-term neotectonic activity obtained from two caves localized in the eastern part of the Slovensky kras Mts. (SE Slovakia) show generally NE-SW oriented dilatation. This orientation is in a good accordance with the orogen-parallel extension monitored in the Western Carpathians. Differing short-lasting trends were distinguished in 2011-2012 and 2013-2015, which supports the significance of the tectonic pulse at the end of 2012 and the beginning of 2013. Moreover, simultaneous short-lasting faulting occurred at both sites under the transtensional tectonic regime, where the principal maximum compressional axis operated in a NW-SE direction (sigma(1)). The observed results were compared to data from monitoring points in distant areas of the European plate. Workplace Institute of Rock Structure and Mechanics Contact Iva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216 Year of Publishing 2019 Electronic address https://www.irsm.cas.cz/materialy/acta_content/2018_doi/Briestensky_AGG_2018_0007.pdf
Number of the records: 1