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Geodetic surveys in detection of geological features: a case study of Inowrocław area, central Poland

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Języki publikacji
EN
Abstrakty
EN
Remotely obtained geodetic survey data can be used to detect anomalies in the terrain surface over different geological structures, like faults or deposit boundaries. Some computer techniques are helpful to extract the influence of geological phenomena on typical distribution of the measured elevations. Certain disturbances in profile lines can be considered as additional, human-induced effects or caused by geological processes. The paper demonstrates such an analysis basing on geodetic data with some support of geophysical results. The examined morphological profiles and profiles of subsidence bowls caused by mining in the area of Inowroclaw (central Poland) illustrate the problem of an underestimated mechanism in non-geological disciplines. For geologists this is another example of environmental interaction between relief-forming processes and subsurface conditions. Furthermore, it brings additional information about processes of mining subsidence, which is the primary topic of this study. Mutual relationships between vertical displacements induced by mining or other factors and morphological profiles point to the dominant role played by mobility of geological structures, as shown by correlation between geodetic and geophysical data.
Rocznik
Strony
169--176
Opis fizyczny
bibliogr. 12 poz., rys., wykr.
Twórcy
  • Faculty of Mining Surveying and Environmental Engineering, AGH University of Science and Technology, Al. Mickiewicza 30, 30-059 Kraków, Poland, szczerbo@uci.agh.edu.pl
Bibliografia
  • Budryk, W., 1933. Zapadliska na terenie miasta Inowrocławia. (In Polish). Przegląd Górniczo-Hutniczy, 8: 1-4, Sosnowiec.
  • Bujakowski, W., 1986. Geological mapping study of northern part of Inowrocław salt dome. (In Polish, English summary). Zeszyty Naukowe AGH, Kwartalnik Geologia, No. 10/4, pp. 121-130.
  • EN 1997Eurocode 7. Geotechnical design. BSI British Standards. 2004.
  • Molewski, P., 2007. Neotectonic andglacidynamic conditions for the formation ofthe Pleistocene of the Kujawy Moraine Plateau. (In Polish, English summary). Wydawnictwo Naukowe Uniwersytetu Mikołaja Kopernika, Toruń, 140 pp.
  • Molewski, P., 2008. Zastosowanie metod geostatystycznych do badań ruchów neotektonicznych (halokinetycznych) na obszarze Wysoczyzny Kujawskiej. (In Polish). Landform Analysis, 9: 361-363.
  • Niewiarowski, W., 1983. Postglacial vertical movements of the Earth's crust in the Kujavian Lake District (Pojezierze Kujawskie) in the light of geomorphological research. (In Polish, English summary). Przegląd Geograficzny, 55: 13-31.
  • Pilecki, Z., Szczerbowski, Z., Kłosiński, J. & Koster, M., 2003. Seismic estimation of rock mass state over salt dome Inowrocław. (In Polish, English summary). Bezpieczeństwo Pracy i Ochrona Środowiska w Górnictwie, 5 (105): 48-50.
  • Szczerbowski, Z., 2003. Mining and geological conditions of deformation of Saint Mary's Church building in Inowrocław. (In Polish, English summary). AGH, Geodezja, 9 (2/1): 529-536.
  • Szczerbowski, Z., 2004. Preliminary results of geodetic measurements in the Inowrocław salt dome area, central Poland. Annales Societatis Geologorum Poloniae, 74: 319-324.
  • Tarka, R., 1988. Postglacial rise of salt diapirs at Inowrocław and Góra - a phenomenon quickness. (In Polish, English summary). Przegląd Geologiczny, 36 (2): 105-106.
  • Tarka, R., 1991. The tectonic evolution of Polish salt diapirs. Bulletin of the Polish Academy of Sciences, Earth Sciences, 39: 85-91.
  • Tarka, R., 1992. Tectonics of some salt deposits in Poland based on mesostructural analysis. (In Polish, English summary). Prace Państwowego Instytutu Geologicznego, 137: 1-47.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS7-0001-0023
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