PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Quaternary fault activity in the SW Pannonian Basin : GPR surveying in the Bilogora Mt. (NE Croatia)

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
In areas experiencing low deformation rates, landscapes provide limited evidence of ongoing tectonic activity, being either masked or altered by exogenic processes. Accordingly, the identification of fault activity and near surface deformation is commonly accomplished by multidisciplinary research combining geological, geophysical and geomorphic methods. In this study, Quaternary fault activity in the SW Pannonian Basin is investigated in the region of Bilogora, NE Croatia. The study area is positioned along the SW margin of the Drava Depression that was uplifted during the Pliocene and Quaternary within the Drava Depression Boundary Fault Zone. In this fault zone six GPR profiles were recorded. Reflection patterns, radar facies and truncations determined fault activity and near-surface deformation at four locations with vertical displacements of ≤1 m. At two sites, profiles did not show truncation of the shallowest reflections, however, an elevation difference of ca. 10 m between two palaeostream channels along one of the profiles suggests Quaternary uplift accommodated by a mapped fault. Considering the importance of the seismogenic potential of active faults and their correlation with the seismicity of Bilogora, this research will be followed by additional studies of near-surface strata deformation and palaeoseismological fault properties.
Rocznik
Strony
19--38
Opis fizyczny
Bibliogr. 68 poz., rys., tab., wykr.
Twórcy
autor
  • University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Department of Geology and Geological Engineering, Pierottijeva 6, 10000 Zagreb, Croatia
autor
  • University of Ljubljana Faculty of Natural Sciences and Engineering, Aškerčeva c. 12, 1000 Ljubljana, Slovenia
autor
  • University of Zagreb, Faculty of Geodesy, Kačićeva 26, 10000 Zagreb, Croatia
  • University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Department of Geology and Geological Engineering, Pierottijeva 6, 10000 Zagreb, Croatia
autor
  • University of Ljubljana Faculty of Natural Sciences and Engineering, Aškerčeva c. 12, 1000 Ljubljana, Slovenia
Bibliografia
  • 1. Alasset, P.J., Meghraoui, M., 2005. Active faulting in the western Pyrenees (France) - paleoseismic evidence for late Holocene ruptures. Tectonophysics, 409: 39-54.
  • 2. Anderson, K.B., Spotila, J.A., Hole, J.A., 2003. Application of geomorphic analysis and ground-penetrating radar to characterization of paleoseismic sites in dynamic aliuvial environments: an example from southern California. Tectonophysics, 368: 25-32.
  • 3. Babič, Ž., Čakarun, I., Sokač, A., Mraz, V., 1978. Geology of the Quaternary deposits of Drava River (in Croatian). Geološki Vjesnik, 30: 43-61
  • 4. Bada, G., Horvath, F., Gerner, P., Fejes, I., 1999. Review of the present-day geodynamics of the Pannonian basin: progress and problems. Journal of Geodynamics, 27: 501-527.
  • 5. Bada, G., Horváth, F., Dovényi, P., Szafián, P., Windhoffer, G., Cloetingh, S., 2007. Present-day stress field and tectonic inversion in the Pannonian basin. Global and Planetary Change, 58: 165-180.
  • 6. Csontos, L., Voros, A., 2004. Mesozoic plate tectonic reconstruction of the Carpathian region. Palaeoclimatology, Palaeoecology, Palaeogeography, 210: 156.
  • 7. Crnko, J. (unpublished). Basic geological map of Kutina, M 1:100 000 (in Croatian). Geological Survey Zagreb, Zagreb.
  • 8. Ferry, M., Meghraoui, M., Girard, J., Rockwell, T.K., Kozaci, O., Akyuz, S., Barka, A., 2004. Ground penetrating radar investigations along the North Anatolian fault near Izmit, Turkey: constraints on the rightlateral movement and slip history. Geology, 32: 85-88.
  • 9. Fodor, L., Jelen, B., Márton, E., Skaberne, D., Čar, J., Vrabec, M., 1998. Miocene-Pliocene tectonic evolution of the Slovenian Periadriatic fault: implications of Alpine-Carpathian extrusion models. Tectonics, 17: 690-709.
  • 10. Fodor, L., Bada, G., Csillag, G., Horváth, E., Ruszkiczay-RUdiger, Z., Palotás, K., Síkhegyi, F., Timár, G., Cloetingh, S., Horváth, F., 2005. An outi ine of neotectonic structures and morphotectonics of the western and ceniral Pannonian Basin. Tectonophysics, 410: 15-41.
  • 11. Galović, I., Marković, S., 1979. Basic geological map of Virovitica, M 1:100 000 (in Croatian). Geological Survey Zagreb, Federal Geological Institute, Beograd.
  • 12. Galović, I., Marković, S., Magdalenie, Z., 1981. Explanatory notes for Basic geological map of Virovitica (1:100 000) (in Croatian). Federal Geological Institute, Beograd.
  • 13. Grant, J.A., Schultz, P.H., 1996. Ground penetrating radar deployment in Argentine loess: implications for the character of the Martian stealth region. Lunar and Planetary Science, 27: 445-446.
  • 14. Hećimović, I., 1986. Basic geological map of Đurđevac, M 1:100000 (in Croatian). Geological Survey Zagreb, Federal Geological Institute Beograd.
  • 15. Hećimović, I., 1987. Explanatory notes for geological map of Đurđevac (1:100 000) (in Croatian). Federal Geological Institute, Beograd.
  • 16. Hećimović, I., 1995. Structure of the border area of Mt. Kalnik (in Croatian). Ph.D. thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb.
  • 17. Herak, D., Herak, M., Tomljenović, B., 2009. Seismicity and earthquake focal mechanisms in North-Western Croatia. Tectonophysics, 465: 212-220.
  • 18. Horváth, F., Tari, G., 1999. IBS Pannonian Basin project: a review of the main results and their bearings on hydrocarbon exploration. Geological Society Special Publications, 156: 195-213.
  • 19. Jamičić, D., Brkić, M., 1987. Basic geological map of Orahovica, M 1:100 000 (in Croatian). Geological Survey Zagreb, Federal Geological Institute, Beograd.
  • 20. Jamičić, D., 1989. Basic geological map of Daruvar, M 1:100 000 (in Croatian). Geological Survey Zagreb, Federal Geological Institute, Beograd.
  • 21. Jamšek, P., Benedetti, L., Bavec, M., Atanackov, J., Vrabec, M., Gosar, A., 2011a. Preliminary report on the Vodice fault activity and its potential for seismic hazard in the Ljubljana Basin, Slovenia. In: Proceedings: 2nd INQUA-IGCP-567 International Workshop on Active Tectonics, Earthquake Geology, Archaeology and Engineering, Corinth, Greece, 19-24 September 2011, (Proceedings volume 2, 2011: Earthquake Geology and Archaeology: Science, Society and Critical Facilities) (ed. C. Grutzner et al.): 96-98. Corinth, 2nd INQUA-IGCP-567, International Workshop.
  • 22. Jamšek, P., Benedetti, L., Bavec, M., Atanackov, J., Gosar, A., Zajc, M., Vrabec, M., 2011b. Tectonic activity and seismogenic potential of the Vodice fault: surface and subsurface evidence. Geološki Zbornik, 21: 36-38.
  • 23. Jamšek Rupnik, P., 2013. Geomorphological evidence of active tectonics in the Ljubljana basin. Ph.D. thesis, University of Ljubljana, Faculty of Natural Sciences and Engineering, Ljubljana.
  • 24. Jarosiński, M., Beekman, F., Matenco, L., Cloetingh, S., 2011. Mechanics of basin inversion: finite element modeling of the Pannonian Basin System. Tectonophysics, 502: 121-145.
  • 25. Jol, H.M., 2009. Ground Penetrating Radar: Theory and Applications. Elsevier Science, Amsterdam, Oxford.
  • 26. Korolija, B., Crnko, J., 1985. Basic geological map of Bjelovar, M 1:100 000 (in Croatian). Geological Survey Zagreb, Federal Geological Institute, Beograd.
  • 27. Korolija, B., Vragović, M., Crnko, J., Mamužić, P., 1986. Explanatory notes for geological map of Bjelovar (1:100 000) (in Croatian). Federal Geological Institute, Beograd.
  • 28. Kranjec, V., Prelogović, E., Hernitz, Z., Blašković, I., 1971. Lithofacies relations in late Neogene and Quaternary deposits in the area of Bilogora-Northern Croatia (in Croatian). Geološki Vjesnik, 24: 47-56.
  • 29. Lenkey, L., Dovényi, P., Horváth, F., Cloetingh, S.A.P.L., 2002. Geothermic of the Pannonian basin and its bearing on the neotectonics. EGU Stephan Mueller Special Publication Series, 3: 29-40.
  • 30. Lučić, D., Saftić, B., Krizmanić, K., Prelogović, E., Britvić, V., Mesić, I., Tadej, J., 2001. The Neogene evolution and hydrocarbon potential of the Pannonian Basin in Croatia. Marine and Petroleum Geology, 18: 133-147.
  • 31. Malá, 2009. Malá ProEx- Operating manual-Professional Explorer Control Unit. MALÄ Geoscience AB, Malá, Sweden.
  • 32. Malvić, T., 2003. Oil-geological relations and probability of discovering new hydrocarbon reserves in the Bjelovar Sag (in Croatian). Ph.D. thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb.
  • 33. Malvić, T., Velić, J., 2011. Neogene tectonics in Croatian part of the Pannonian Basin and reflectance in hydrocarbon accumulations. In: New Frontiers in Tectonic Research-At the Midst of Plate Convergence (ed. U. Schattner): 215-238. InTech.
  • 34. Marjanović, M., 2010. CROPOS-Croatian coordinate system (in Croatian), Ekscentar, 12: 28-34.
  • 35. Marjanović, M., Link, H-P., 2011. CROPOS-Us ers' Manual. State Geodetic Administration (Republic of Croatia), Zagreb, Croatia: ISB N :978-953-293-100-6
  • 36.Markovič, S., 1985. Basic geological map of Podravska Slatina, M 1:100 000 (in Croatian). Geological Survey Zagreb, Federal Geological Institute, Beograd.
  • 37. Marković, S., 1986. Explanatory notes for geological map of Podravska Slatina (1: 100 000) (in Croatian). Federal Geological Institute Beograd.
  • 38. Matoš, B., 2014. Neotectonic and recently active faults in Bilogora Mountain area and assessment of their seismogenic potential (in English). Ph.D. thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb.
  • 39. Matoš, B., Tomljenović, B., Pérez-Peńa, J.V., 2016. Landscape response to recent tectonic deformation in the SW Pannonian Basin: evidence from DEM based morphometric analysis of Bilogora Mt. area, NE Croatia. Geomorphology, 263: 132-155.
  • 40. McCalpin, J.P., ed., 2009. Paleoseismology. International Geophysics Series, 95, Burlington (MA), Academic Press, Elsevier.
  • 41. McClymont, A.F., Green, A.G., Kaiser, A., Horstmeyer, H., Langridge, R., 2010. Shalt ow fault segmentation of the Alpine fault zone, New Zea land revealed from 2-D and 3-D GPR surveying. Journal of Applied Geophysics, 70: 343-354.
  • 42. Meschede, M., Aspiron, U., Reicherter, K., 1997. Visualization of tectonic structures in shallow-depth high-resolution ground penetrating radar (GPR) profiles. Terra Nova, 9: 167-170.
  • 43. Nagymarosy, A., Muller, P., 1988. Some aspects of Neogene biostratigraphy in the Pannonian Basin. AAPG Memoir, 45: 58-68.
  • 44. Neal, A., 2004. Ground-penetrating radar and its use in sedimentology: principles, problems and progtess. Earth-Science Reviews, 66: 261-330.
  • 45. Patidar, A.K., Maurya, D.M., Thakkar, M.G., Chamayal, L.S., 2007. Fluvial geomporphology and neotectonic activity based on field and GPR data, Katrol hill range, Kachchh, Western India. Quaternary International, 159: 74-92.
  • 46. Pikija, M., 1987. Basic geological map of Sisak, M 1:100 000 (in Croatian). Geological Survey Zagreb, Federal Geological Institute, Beograd.
  • 47. Prelogović, E., 1974. Neotectonic and structural relations in Drava region (in Croatian). Ph.D. thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb.
  • 48. Prelogović, E., Velić, J., 1988. Quaternary tectonic activity in the Western part of Drava Depression (in Croatian). Geološki Vjesnik, 41: 237-253.
  • 49. Prelogović, E., Velić, J., 1992. Correlation of Quaternary sediments and tectonic activity of the eastern part of the Drava River Depression. Geologia Croatica, 45: 151-162.
  • 50. Prelogović, E., Hernitz, Z., Blašković, I., 1969. Application of morphometric methods in solving structural and tectonic relations in Bilogora-Northern Croatia (in Croatian). Geološki Vjesnik, 22: 525-531.
  • 51. Prelogović, E., Saftić, B., Kuk, V., Velić, J., Dragaš, M., Lučić, D., 1998. Tectonic activity in the Croatian part of the Pannonian basin. Tectonophysics, 297: 283-293.
  • 52. Rashed, M., Kawamura, D., Nemoto, H., Miyata, T., Nakagawa, K., 2003. Ground penetrating radar investigations across the Uemachi fault, Osaka, Japan. Journal of Applied Geophysics, 53: 63-75.
  • 53. Ratschbacher, L., 1991. Lateral extrusion in the Eastern Alps, Part 1: Boundary conditions and experiments scaled for gravity, Part 1: Structural analysis. Tectonics, 10: 245-256.
  • 54. Ratschbacher, L., Frisch, W., Linzer, H.-G., Merle, O., 1991. Lateral extrusion in the Eastern Alps, part 2: Structural analysis. Tectonics, 10: 257-271.
  • 55. Rögl, F., 1999. Mediterranean and Paratethys. Facts and hypotheses of an Oligocene to Miocene paleogeography (short overt view). Geologica Carpathica, 50: 339-349.
  • 56. Royden, L.H., Horváth, F., eds., 1988. The Pannonian Basin - a study in basin evolution. AAPG Memoir, 45.
  • 57. Saftić, B., Velić, J., Sztanó, O., Juhász, G., Ivković, Ž., 2003. Tertiary subsurface facies, source rocks and hydrocarbon reservoirs in the SW part of the Pannonian Basin (Northern Croatia and South-Western Hungary). Geologia Croatica, 56: 101-122.
  • 58. Sandmeier, K.J., 2011. REFLEXW Version 6.0, Windows 9x/NT/2000/XP/7. Program for the processing of seismic, acoustic or electromagnetic reflection, refraction and trans mission data. Software Manual, Karlsruhe, Germany.
  • 59. Steininger, F.F., Wessely, G., 1999. From the Tethyan Ocean to the Paratethys Sea: Oligocene to Neogene stratigraphy, paleogeography and paleobiogeography of the circum-Mediterranean region and the Oligocene to Neogene basin evolution in Austria. Mitteilungen der Osterreichischen Geologischen Gesellschaft, 92: 95-116.
  • 60. Šimunić, A., Hećimović, I., Avanić, R., 1994. Basic geological map of Koprivnica, M 1:100 000 (in Croatian). Geological Survey Zagreb, Zagreb.
  • 61. Tari, V., Pamić, J., 1998. Geodynamic evolution of the northern Dinarides and the southern part of the Pannonian Basin. Tectonophysics, 297: 269-281.
  • 62. Tari, G., Dovényi, P., Dunkl, I., Horváth, F., Lenkey, L., Stefanescu, M., Szafián, P., Tóth, T., 1999. Litosphere structure of the Pannonian basin de fived from seismic, gravity and geothermal data. Geological Society Special Publications, 156: 215-250.
  • 63. Tomljenović, B., Csontos, L., 2001. Neogene-Quaternary structures in the border zone between Alps, Dinarides and Pannonian Basin (Hrvatsko zagorje and Karlovac Basin, Croatia). International Journal of Earth Sciences (Geologische Rundschau), 90: 560-578.
  • 64. Ustaszewski, K., Schmid, S.M., FUgenschuh, B., Tischler, M., Kissling, E., Spakman, W., 2008. A map-view restoration of the Alpine-Carpathian-Dinaridic system for Early Miocene. Swiss Journal of Geosciences, 101 (Supplement 1): 273-294.
  • 65. Velić, J., Weisser, M., Saftić, B., Vrbanac, B., Ivković, Ž., 2002. Petroleum-geological characteristics and exploration level of the three Neogene depositional megacycles in the Croatian part of the Pannonian basin. Nafta, 53: 239-249.
  • 66. Zajc, M., 2015. Optimization of Low-Frequency Ground Penetrating Radar surveys for the characterization of shallow geological structures (in Slovenian). Ph.D. thesis, University of Ljubljana, Faculty of Civil and Geodetic Engineering, Ljubljana.
  • 67. Zajc, M., Pogačnik, Ž., Gosar, A., 2014. Ground penetrating radar and structural geological mapping investigation of karstand tectonic features in flyschoid rocks as geological hazard for exploitation. International Journal of Rock Mechanics and Mining Sciences, 67: 78-87.
  • 68. Zajc, M., Celarc, B., Gosar, A., 2015 . Structural-geological and karst feature investigations of the limestone-flysch thrust-fault contact using low-frequency ground penetrating radar (Adriai -Dinarides thrust zone, SW Slovenia). Environmental Earth Sciences, 73: 8237-8249.
Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-861a5987-1dd6-4358-8f3d-fc667eae2318
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.