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Near-surface Structure of the Carpathian Foredeep Marginal Zone in the Roztocze Hills Area

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Języki publikacji
EN
Abstrakty
EN
Shallow seismic survey was made along 1280 m profile in the marginal zone of the Carpathian Foredeep. Measurements performed with standalone wireless stations and especially designed accelerated weight drop system resulted in high fold (up to 60), long offset seismic data. The acquisition has been designed to gather both high-resolution reflection and wide-angle refraction data at long offsets. Seismic processing has been realised separately in two paths with focus on the shallow and deep structures. Data processing for the shallow part combines the travel time tomography and the wide angle reflection imaging. This difficult analysis shows that a careful manual front mute combined with correct statics leads to detailed recognition of structures between 30 and 200 m. For those depths, we recognised several SW dipping tectonic displacements and a main fault zone that probably is the main fault limiting the Roztocze Hills area, and at the same time constitutes the border of the Carpathian Forebulge. The deep interpretation clearly shows a NE dipping evaporate layer at a depth of about 500-700 m. We also show limitations of our survey that leads to unclear recognition of the first 30 m, concluding with the need of joint interpretation with other geophysical methods.
Czasopismo
Rocznik
Strony
179--189
Opis fizyczny
Bibliogr. 32 poz.
Twórcy
  • Institute of Geophysics, Polish Academy of Sciences, Warsaw, Poland
autor
  • Institute of Geophysics, Polish Academy of Sciences, Warsaw, Poland
autor
  • Institute of Geophysics, Polish Academy of Sciences, Warsaw, Poland
autor
  • Faculty of Geology, University of Warsaw, Warsaw, Poland
autor
  • Faculty of Geology, University of Warsaw, Warsaw, Poland
Bibliografia
  • 1. Bąbel M (2004) Badenian evaporite basin of the northern Carpathian Foredeep as a drawdown salina basin. Acta Geol Pol 54(3):313–337
  • 2. Bachrach R, Nur A (1998) High-resolution shallow seismic experiments in sand, part I: water table, fluid flow and saturation. Geophysics 63(1):1225–1233. https://doi.org/10.1190/1.1444423
  • 3. Bruno PP, Improta L, Castiello A, Villani F, Montone P (2010) The Vallo di Diano fault system: new evidence for an active range-bounding fault in Southern Italy using shallow, high-resolution seismic profiling. Bull Seismol Soc Am 100(2):882–890
  • 4. Bruno PP, Castiello A, Villani F, Improta L (2013) High-resolution densely spaced wide-aperture seismic profiling as a tool to aid seismic hazard assessment of fault-bounded intramontane basins: application to Vallo di Diano, Southern Italy. Bull Seismol Soc Am 103(3):1969–1980
  • 5. Buker F, Green AG, Horstmeyer H (1998) Shallow seismic reflection study of a glaciated valley. Geophysics 63:1395–1407
  • 6. Dusar M, Rijpens J, Sintubin M, Wouters L (2001) Plio-Pleistocene fault pattern of the Feldbiss fault system (southern border of the Roer Valley Graben, Belgium) based on high resolution reflection seismic data. Neth J Geosci 80:79–93
  • 7. Feroci M, Orlando L, Balia E, Bosman C, Cardarelli E, Deidda G (2000) Some considerations on shallow seismic reflection surveys. J Appl Geophys 45:127–139
  • 8. Francese RG, Hajnal Z, Schmitt D, Zaja A (2007) High resolution seismic reflection imaging of complex stratigraphic features in shallow aquifers. Memorie Descrittive della Carta Geologica d’Italia, LXXVI, pp 175–192
  • 9. Green AG, Campbell FM, Kaiser AE, Dorn C, Carpentier S, Doetsch JA, Horstmeyer H, Nobes D, Campbell J, Finnemore M, Jongens R, Ghisetti F, Gorman AR, Langridge RM, McClymont AF (2010) International Conference on Environmental and Engineering Geophysics, p 15
  • 10. Hobro JWD (1999) Three-dimensional tomographic inversion of combined reflection and refraction seismic travel-time data. Ph.D. Thesis, Department of Earth Sciences, University of Cambridge, Cambridge, UK
  • 11. Jankowski L, Margielewski W (2015) Pozycja tektoniczna Roztocza w świetle historii rozwoju zapadliska przedkarpackiego. Biuletyn Państwowego Instytutu Geologicznego 462:7–28
  • 12. Jaroszewski W (1977) Synsedymentacyjne przejawy mioceńskiej ruchliwości tektonicznej na Roztoczu Środkowym. Przegląd Geologiczny 25(8/9):418–427
  • 13. Kondracki J (1994) Geografia Polski, mezoregiony fizyczno-geograficzne, PWN
  • 14. Krzywiec P (2001) Contrasting tectonic and sedimentary history of the central and eastern parts of the Polish Carpathian Foredeep basin—results of seismic data interpretation. Mar Pet Geol 18:13–38
  • 15. Kurkowski S (1998) Szczegółowa Mapa Geologiczna Polski 1:50 000, arkusz Józefów. Państwowy Instytut Geologiczny
  • 16. Majdański M, Trzeciak M, Gaczyński E, Maksym A (2016) Seismic velocity estimation from post-critical wide-angle reflections in layered structures. Stud Geophys Geod 60:565–582
  • 17. Malinowski M, Guterch A, Narkiewicz M, Probulski J, Maksym A, Majdański M, Środa P, Czuba W, Gaczyński E, Grad M, Janik T, Jankowski L, Adamczyk A (2013) Deep seismic reflection profile in Central Europe reveals complex pattern of Paleozoic and Alpine accretion at the East European Craton margin. Geophys Res Lett 40:1–6
  • 18. Myśliwiec M (2004) Mioceńskie skały zbiornikowe zapadliska przedkarpackiego. Przegląd Geologiczny 52:581–592
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  • 21. Robertsson JOA, Holliger K, Green AG, Pugin A, De Iaco R (1996) Effects of near-surface waveguides on shallow high resolution seismic refraction and reflection data. Geophys Res Lett 23:495–498
  • 22. Roniewicz P, Wysocka A (1999) Charakterystyka sedymentologiczna utworów środkowomioceńskich północno-wschodniej, brzeżnej strefy zapadliska przedkarpackiego. Prace Państwowego Instytutu Geologicznego, CLXVIII, pp 83–97
  • 23. Steeples DW (2000) A review of shallow seismic methods. Ann Geofis43:1021–1030
  • 24. Steeples DW, Miller RD (1990) Seismic reflection methods applied to engineering, environmental, and groundwater problems. In: Ward SW (ed) Geotechnical and environmental geophysics, vol 3, Society of Exploration Geophysicists, no 5, pp 1–30
  • 25. Steeples DW, Miller RD (1998) Avoiding pitfalls in shallow seismic reflection surveys. Geophysics 63:1213–1224
  • 26. Sugiyama Y, Mizuno K, Nanayama F, Sugai T, Yokota H, Hosoya T, Miura K, Takemura K, Kitada N (2003) Study of blind thrust faults underlying Tokyo and Osaka urban areas using a combination of high-resolution seismic reflection profiling and continuous coring. Ann Geophys 46:1071–1085
  • 27. Vesnaver AL, Gohm G, Madrussani G, Petersen SA, Rossi G (1999) Tomographic imaging by reflected and refracted arrivals at the North Sea. Geophysics 64:1862–1952
  • 28. Wysocka A (2006) Klastyczne utwory badeńskie Roztocza—przebieg sedymentacji w północnej marginalnej strefie basenu zapadliska przedkarpackiego. Przegląd Geologiczny 54:430–437
  • 29. Wysocka A, Jasionowski M (2006) Polish part of Roztocze Hills. POKOS Materiały Konferencyjne 11–14
  • 30. Wysocka A, Krzywiec P, Maksym A (2006) Kamieniołom Józefów. POKOS Materiały Konferencyjne 19–24
  • 31. Wysocka A, Radwański A, Górka M, Bąbel M, Radwańska U, Złotnik M (2016) The middle miocene of the fore-Carpathian Basin (Poland, Ukraine and Moldova). Acta Geol Pol 66:351–401
  • 32. Zelt CA (1999) Modelling strategies and model assessment for wide-angle seismic traveltime data. Geophys J Int 139:183–204
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018)
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-38cafd15-6de2-4781-8d3e-60f3f29efb09
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