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Field mapping of buried faults : a new approach applied in the Western Carpathians

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Fault array in an area covered by Quaternary sediments and deprived of bedrock outcrops was investigated using fault trace mapping by geophysical methods and human feedback information from dowsing. The tectonics in the study area is dominated by a ENE-WSW fault zone affecting regional-scale structures. The fault network was approximated by dowsing-enhanced mapping and subsequently confirmed by field geophysical measurements using electromagnetic and radon emanometry methods. A resultant detailed map of structural discontinuities highlighted that combined dowsing and geophysical survey is an effective and reliable tool to identify buried faults. This approach with its low costs and fast field recognition is highly recommended for construction-work planning and for mineral resources exploration and exploitation.
Słowa kluczowe
Rocznik
Strony
35--46
Opis fizyczny
Bibliogr. 26 poz., rys., wykr.
Twórcy
autor
  • Comenius University, Faculty of Sciences, Department of Geology and Paleontology, Mlynská dolina G, 842 15 Bratislava, Slovakia
autor
  • Comenius University, Faculty of Sciences, Department of Mineralogy and Petrology, Mlynská dolina G, 842 15 Bratislava, Slovakia
autor
  • Comenius University, Faculty of Sciences, Department of Applied and Environmental Geophysics, Mlynská dolina G, 842 15 Bratislava, Slovakia
autor
  • Comenius University, Faculty of Sciences, Department of Applied and Environmental Geophysics, Mlynská dolina G, 842 15 Bratislava, Slovakia
autor
  • Comenius University, Faculty of Sciences, Department of Applied and Environmental Geophysics, Mlynská dolina G, 842 15 Bratislava, Slovakia
Bibliografia
  • 1. Beidinger, A., Decker, K., 2011. 3D geometry and kinematics of the Lassee flower struc ture: im pli ca tion for seg men ta tion and seismotectonics of the Vienna Basin strike-slip fault, Austria. Tectonophysics, 499: 22-40.
  • 2. Betz, H.D., 1995. Unconventional water detection. Field test of dowsing technique in dry zones: part 2. Journal of Scientific Exploration, 9: 159-189.
  • 3. Born, I.A., 1774. Briefe über Mineralogische Gegenstände, auf seiner Reise durch das Temeswarer Bannat, Siebenbürgen, Ober und Nieder-Hungarn, Frankfurt a/Main Leipzig, Briefe: 1-22.
  • 4. Daniel, J., 1999. Geophysical factors of an environment. A natural radioactivity (in Slovak). MŽP SR, Uranpress, Spišská Nová Ves, unpublished report.
  • 5. Daynes, J., 2012. The Dowsing and Geophysics Project at Moistown, Broadwoodkelly. Interim report 2012, ACE Archaeology Club, Great Britain.
  • 6. Fiddick, T., 2011. Dowsing: With an Account of Some Original Experiments. The Cornovia Press, Sheffield, United Kingdom.
  • 7. Giammanco, S., Imme, G., Mangano, G., Morelli, D., Neri, M., 2009. Comparison between different methodologies for detecting radon in soil along an active fault: the case of the Pernicana fault system, Mt. Etna (Italy). Applied Radiation and Isotopes, 67: 178-185.
  • 8. Grecula, P., Bartalský, J., Cambel, B., Herčko, I., Kaličiak, M., Matula, M., Melioris, L., Polakovič, D., Slavkay, M., Sombathy, L., Šefara, J., 2006. History of geology in Slovakia (in Slovak). Štátny geologický ústav Dionýza Štúra, Bratislava.
  • 9. Gruntorád, J., Mazáč, O., 1994. Impact of subt le dynamic geofactors on environment. Acta Universitatis Carolinae Environ- mentalica, 8: 3-53.
  • 10. Janků, J., Pospíšil, L., Vass, D., 1984. A contribution of remote sensing methods to the knowledge of the Western Carpathians geological structure (western segment) (in Slovak). Mineralia Slovaca, 16: 121-137.
  • 11. Kowalski, W.C., 1996. Dowsing and radiesthesia; to test or not to test, that is the question (in Polish with English summary). Przegląd Geologiczny, 44: 39-42.
  • 12. Landa, V.E., Kovalevsky, A.L., 1997. Integration of dowsing with biogeochemical and electrical prospecting techniques at gold ore deposits. Bulletin of Dowsing, 8: 9-12.
  • 13. Lohmann, H.H., 1998. Dowsing versus geophysics. Bulletin for Applied Geology, 3: 199-203.
  • 14. Mahel’, M., 1969. Faults and their role in the Mesozoics of the Inner Carpathians (in Slovak). Geologické práce, Správy, 47: 7-29.
  • 15. Mahel’, M., Kamenický, J., Fusán, O., Matějka, A., 1967. Regional geology of the ČSSR (in Czech). Nakl. ČSAV Praha.
  • 16. Marko, F., 2012. Cenozoic stress field and fault í ng at the northern margin of the Danube basin (Western Carpathians, Slovakia) (in Slovak with English summary). Mineralia Slovaca, 44: 213-230.
  • 17. Marko, F., Kováč, M., 1997. Folded Kiscellian turbidites - the evidence of dextral wrenching within ENE-WSW striking shear zone (Hrabník, Malé Karpaty Mts., Western Carpathians). AAPG Bulletin, 81: 1398.
  • 18. Marko, F., Kováč, M., Fodor, L., Šútovská, K., 1990. Deformation and kinematics of the Miocene shear zone in the northern part of the Malé Karpaty Mts. (Buková furtow, Hrabník formation) (in Slovak with English summary). Mineralia Slovaca, 22: 399-410.
  • 19. Marko, F., Dyda, M., Kóša, J., Silva, A.M., Daudi, E.X.F., Sénvano, A.S., Tembe, S.S., Machado, G., 2006. Hydrogeological environment of the Lebombo monocline (Provi nce Maputo). Abstract volume, 21st Colloquium on African Geology, 03-06 2006 Maputo: 363-364.
  • 20. Marko, F., Túnyi, I., Andriessen, P.A.M., Fojtíková, L., Piovarči, M., Králiková, S., 2013. Carpathian Shear Corridor - a zone of blocks uplift, tilting, rotation and recent seismic activity (Western Carpathians).GEEWEC2013 “Geological evolution of the Western Carpathians: new ideas in the field of inter-regional correlations”, Smolenice, Slovakia, October 16.-19.2013, Abstract Book, (ISBN 978-80-971442-5-8): 59-60.
  • 21. Michalik, J., 1984. Some remarks on developmental and structural interpretation of the Northwestern part of the Malé Karpaty Mts. (Western Carpathians). Geologický Zborník, Geologica Carpathica, 33: 481-507.
  • 22. Moldovan, I.A., Apostol, A., Moldovan, A., Ionescu, C., Placinta, A.O., 2013. The biolocation method used for stress forecast ing in Vrancea (Romania) seismic zone. Romanian Reports in Physics, 65: 261-270.
  • 23. Plašienka, D., 1990. Regional shear and transpression zones in the Tatric unit of the Malé Karpaty Mts. (in Slovak). Mineralia Slovaca, 22: 55-62.
  • 24. Polák, M., Plašienka, D., Kohút, M., Putiš, M., Bezák, V., Filo, I., Olšavský, M., Havrila, M., Buček, S., Maglay, J., Elečko, M., Fordinál, K., Nagy, A., Hraško, L., Németh, Z., Ivanička, J., Broska, I., 2011. Geological map of the Malé Karpaty Mts. region in scale 1:50 000 (in Slovak). MŽP SR, Štátny geologický ústav Dionýza Štúra, Bratislava.
  • 25. Polák, M., Plašienka, D., Kohút, M., Putiš, M., Bezák, V., Maglay, J., Olšavský, M., Havrila, M., Buček, S., Elečko, M., Fordinál, K., Nagy, A., Hraško, L., Németh, Z., Malík, P., Liščák, P., Madarás, J., Slavkay, M., Kubeš, P., Kucharič, L., Boorová, D., Zlínska, A., Síráňová, Z., Žecová, K., 2012. Explanations to geological map of the Malé Karpaty Mts. region in scale 1:50 000 (in Slovak). MŽP SR, Štátny geologický ústav Dionýza Štúra, Bratislava.
  • 26. Pospíšil, L., Nemčok, J., Graniczny, M., Doktór, S., 1986. A contribution of remote sensing methods to identification of faults with lateral movements in the area of the Western Carpathians (in Czech). Mineralia Slovaca, 19: 385-402.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-c98193c2-ee4e-4d9b-a74e-741743f3b7db
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