Warianty tytułu
Języki publikacji
Abstrakty
The paper describes the results of geoelectrical sounding application for the delineation of periglacial structures in Wierzchuca Nagórna within the Drohiczyn Plateau (eastern Poland). The method records the variation of apparent resistivity of deposits along a selected horizontal direction. The survey utilizes a distinct geoelectrical contrast between glacial till and structures composed of sand that have been recognized earlier in the gravel pit wall. The studies have been conducted in direct hinterland of the gravel pit. Rectangular and concentric arrays were applied in the survey. The results have been presented as graphs and resistance distribution maps. The obtained geological image is not complete, although it shows an oriented course of the largest lineaments and traces of a network with a small mesh size (1.5–2 m). The recognized pattern of structures points to harsh climatic conditions during their formation. General orientation of the structures corresponds to the basic elements of the contemporary landscape in the area (slope, valley axes). Geoelectrical sounding using the rectangular array gave better results than in the concentric array, whereas introduction of brine into the system did not enhance the resolution of the readings. The presented resistance distribution maps with a characteristic rhythm of variations may serve as a benchmark for recognizing periglacial structures in areas without exposures.
Czasopismo
Rocznik
Tom
Strony
73--81
Opis fizyczny
Bibliogr. 19 poz., rys.
Twórcy
autor
- Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland, r.mieszkowski@uw.edu.pl
autor
- Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland, j.dzierzek@uw.edu.pl
autor
- Polish Geological Institute – National Research Institute; Rakowiecka 4, 00-975 Warsaw, Poland, dominik.stanczuk@pgi.gov.pl
Bibliografia
- 1. Barry, R., Gan, T. Y., 2011. The global Cryosphere: past, present, and future., Cambridge University Press, ss. 472, New York.
- 2. Dzierżek. J., 2009. Palaeogeography of selected areas in Poland during the Last Glaciation. Acta Geogr. Lodz., 95, ss. 112. (in Polish with English summary)
- 3. Dzierżek, J., Stańczuk, D., 2006. Record and palaeogeographic implications of Pleistocene periglacial processes in the Drohiczyn Plateau, Podlasie Lowland. Geol. Quart., 50 (2), 219-228.
- 4. Fajklewicz, Z., (ed.), 1972. Outline of practice geophysics (Zarys geofizyki stosowanej). Wyd. Geol., ss. 923. (in Polish)
- 5. French, H., 2007. The periglacial environments. 3rd ed., ss. 458, New York, Wiley.
- 6. Jahn, A., 1970. The problem of periglacial zone. (Zagadnienia strefy peryglacjalnej. PWN, ss. 202, Warszawa. (in Polish)
- 7. Jahn, A., 1977. Structures connected with ice wedges in Pleistocene deposits. Studia Geologica Polonica, 52, 177-194.
- 8. Lindner, L., Marks, L., 2012. On the climatostratigraphic scheme of the Middle Polish complex in the Pleistocene of Poland. Prz. Geol., 60, 36–45. (in polish with English summary)
- 9. Mackay, J.R., 1993. Air temperature, snow cover, creep of frozen ground, and the time of ice-wedge cracking, western Arctic coast. Canad. J. Earth Sci., 30, 1720-1729.
- 10. Maizels, J. K., 1986. Frequency of relic frost-fissure structures and prediction of polygon pattern. A quantitative approach. Biul. Perygl., 30, 67-89.
- 11. Marks, L., Pavlovskaya, I. 2004. Extens of Pleistocene glaciations in Eastern Poland and Western Belarus (Zasięgi zlodowaceń plejstoceńskich na obszarze Wschodniej Polski i Zachodniej Białorusi). Mat. XI Konferencja Stratygrafia Plejstocenu Polski, Suprśl, 8-10. (in Polish)
- 12. Marks, L., 2005. Pleistocene glacial limits in the territory of Poland.Prz. Geol., 53 (10/2), 988-993.
- 13. Mieszkowski, R., Porzeżyński, S., 2004. Report on the results of geoelectrical survey in the region of Drohiczyn. (Opracowanie wyników badań geoelektrycznych w rejonie Drohiczyna). Arch. Inst. Geol. Podst. Uniw. Warsz., ss. 6. (in Polish)
- 14. Mieszkowski, R., Porzeżyński, S., 2006. Report on the results of geoelectrical survey in the region of Drohiczyn. Part II. (Opracowanie wyników badań geoelektrycznych w rejonie Drohiczyna. Cz. II.), ss. 8. (in Polish)
- 15. Murton, J., Worsley, B., Goździk, J., 2000. Sand veins and wedges in cold Aeolian environments. Quatern. Sci. Rev., 19, 899-922.
- 16. Nitychoruk, J., Dzierżek, J. Stańczuk, D., 2008a. Detailed Geological Map of Poland in the scale 1: 50 000; Drohiczyn Sheet. (Szczegółowa mapa geologiczna Polski w skali 1 : 50 000 ark. Drohiczyn - 494). Państw. Inst. Geol. (in Polish – electronical document)
- 17. Nitychoruk, J., Dzierżek, J. Stańczuk, D., 2008b. Explanations to the Detailed Geological Map of Poland in the scale 1: 50 000; Drohiczyn Sheet. (Objaśnienia do Szczegółowe mapy geologicznej Polski w skali 1 : 50 000 ark. Drohiczyn - 494). Państw. Inst. Geol., ss. 53 (in Polish – electronical document)
- 18. Stenzel, P., Szymanko, J., 1973. Geophysical methods in hydrogeological and geological-engineering studies. (Metody geofizyczne w badaniach hydrogeologicznych i geologiczno inżynierskich). Wyd. Geol. Warszawa.
- 19. Washburn, A., 1973. Periglacial processes and environments. Edward Arnold. London.
Typ dokumentu
Bibliografia
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Identyfikator YADDA
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