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Tytuł artykułu

The deep-seated lowland relict permafrost from the Suwałki region (NE Poland) : analysis of conditions of its development and preservation

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Treść / Zawartość
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Udryń PIG 1 research borehole drilled in northeastern Poland (54°14’49”N, 23°03’29”E, 223 m a.s.l.) revealed a permafrost layer, at least 93 m thick, within the sedimentary succession below a depth of 357 m. The base of the permafrost has not been reached at 450 m depth, where the drilling stopped, so its total present thickness remains unknown. The relict permafrost, unexpected in this part of Central Europe, is in the ice-water transition phase at a temperature slightly below the 0°C. Analysis of geophysical and hydrogeological data indicates the possibility of preserving the permafrost in the central part of sedimentary cover of the Suwałki Anorthosite Massif over an area of probably 50 km2. Preliminary results of geothermal modelling indicate maximum palaeothickness of permafrost at the end of the Last Glacial Maximum of probably ~600 m. The development of such a thick permafrost results both from a very low average annual temperature in the Weichselian Glaciation and a very low terrestrial heat flow density. It is very probable that similar zones of deep relict permafrost occurrences, undetected so far, may exist in other areas of the Precambrian Platform not only in Poland, but also in the neighbouring countries.
Rocznik
Strony
845--858
Opis fizyczny
Bibliogr. 36 poz., rys., wykr.
Twórcy
autor
  • Polish Geological Institute – National Research Institute, Rakowiecka 4, 00-975, Warszawa, Poland
Bibliografia
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  • 10. Kitover, D.C., van Balen, R.T., Roche, D.M., Vandenberghe, J., Renssen, H., 2013. New estimates of permafrost evolution during the last 21 kyears in Eurasia using numerical modelling. Permafrost and Periglacial Processes, 24: 286-303.
  • 11. Kitover, D.C., van Balen, R.T., Roche, D.M., Vandenberghe, J., Renssen, H., 2015. Advancement toward coupling of the VAMPER permafrost model within the Earth system model iLOVECLIM (version 1.0 description and validation. Geoscientific Model Development, 8: 1445-1460.
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  • 22. Ryka, W., Podemski, M., eds., 1998. Geology of the Suwałki Anorthosite Massif (Northeastern Poland). Prace Państwowego Instytutu Geologicznego, 161: 1-89.
  • 23. Stenni, B., Masson-Delmotte, V., Selmo, E., Oerter, H., Meyere, H., Rothlisberger, R., Jouzel, J., Cattani, O., Falourd, S., Fischer, H., Hoffmann, G., lacumin, P., Johnsen, S.J., Minster, B., Udisti, R., 2010. The deuterium excess records of EPICA Dome C and Dronning Maud Land ice cores (East Antarctica). Quaternary Science Reviews, 29: 146-159.
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  • 25. Szewczyk, J., 2002. Evidences for the Pleistocene-Holocene climatic changes from the deep well temperature profiles from the Polish Lowlands. Proceedings of International Conference: The Earth's Thermal Field and Related Research Methods, Moscow: 271-275.
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  • 29. Szewczyk, J., Gientka, D., 2009. Terrestrial heat flow density in Poland - a new approach. Geological Quarterly, 53 (1): 125-140.
  • 30. Szewczyk, J., Nawrocki, J., 2011. Deep-seated relict permafrost in northeastern Poland. Boreas, 40: 385-388.
  • 31. Szewczyk, J., Gidziński, T., Gientka, D., 2003. Geothermal and hydrogeochemical anomaly at Krzemianka-Udryń area - a remnant of the deep permafrost (in Polish with English summary). Proceedings of the 11th Hydrogeological Symposium, Gdańsk: 229-236.
  • 32. Szewczyk, J., Gidziński, T., Leśniak, P., 2005. Long lasting effects of the deep-seated Weichselian permafrost in the NE of Poland. Transactions of 2nd European Conference on Permafrost, Potsdam (Germany).
  • 33. Szewczyk, J., Nowicki, Z., Gientka, D., 2007. Evaluation of the deep Vistulian permafrost on Polish Lowlands - geothermal and paleohydrogeological implications. Proceedings of the 13th Hydrogeological Symposium, 229-236. Akademia Górniczo-Hutnicza, Kraków-Krynica: 203-211.
  • 34. Šafanda, J., Szewczyk, J., Majorowicz, J., 2004. Geothermal evidence of very low glacial temperatures on a rim of the Fennoscandian ice sheet. Geophysical Research Letters, 31: 1-4, L07211, doi:10.1029/2004GL019547.
  • 35. Velichko, A.A., Nechaev, V.P., Baulin, V.V., Belopukhova, E.S., Danilova, N.S., 2002. Map 2. The Late Valdai-Sartan glacial epoch (in Russian). Permafrost. In: Dynamics of Terrestrial Landscape Components and Inner Marine Basin of Northern Eurasia during the Last 130 000 Years (ed. A.A. Velichko), 5. GEOS Publishers, Moscow.
  • 36. Waller, R.I., Murton, J.B., Kristensen, L., 2012. Glacier-permafrost interactions: processes, products and glaciological implications. Sedimentary Geology, 255: 1-28.
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-7829f068-5b94-41e2-a605-5ed9dba2d677
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