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Identification of a circular structure in eastern Pomerania (northern Poland) : a hypothesis of its origin

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Języki publikacji
EN
Abstrakty
EN
The possible existence of a circular structure in the Kościerzyna region (northern Poland) was suggested in two papers in the 1980s. The current studies were aimed at verifying this hypothesis. Analysis of a digital terrain model of the pre-Quaternary surface relief as well as of the present terrain revealed the existence of a large structure of ca. 50 km in diameter. Its geometry was established based on a model of the Neogene/Pliocene surface and identifiable lineaments. Its characteristic feature is the presence of rim-like forms, an internal plateau, and a “high” in the centre. The structure is estimated to date from before the Pleistocene. The circular structure has been reshaped by glacial erosion and accumulation, and is now buried under Quaternary deposits. The existence of the Kościerzyna circular structure was confirmed by conducted studies, but my hypothesis of an impact origin is still uncertain and needs to be confirmed by future research.
Słowa kluczowe
Rocznik
Strony
205--213
Opis fizyczny
Bibliogr. 46 poz., rys., tab., wykr.
Twórcy
  • Polish Geological Institute – National Research Institute, Marine Geology Branch, Kościerska 5, 80-328, Gdańsk, Poland
Bibliografia
  • 1. Alsouki, M, Riahi, M.A., Yassaghi, A., 2011. Seismic imaging of sub-circular salt-related structures: evidence for passive diapirism in the Straits of Hormuz, Persian Gulf. Petroleum Geoscience, 17: 101-107.
  • 2. Bertoni, C., Cartwright, J.A., 2005. 3D seismic analysis of circular evaporites dissolution structures, Eastern Mediterranean. Journal of the Geological Society, 162: 909-926.
  • 3. Brink, M.C., Waanders, F.B., Bisschoff, A.A., 1997. Vredefort: a model for the anatomy of an astrobleme. Tectonophysics, 270: 83-114.
  • 4. Czapowski, G., Bukowski, K., 2010. Geology and resources of salt deposits in Poland: the state of the art. Geological Quarterly, 54 (4): 509-518.
  • 5. Doktór, M., Graniczny, M., 1983. The ring and circular structures on satelitary images - their meaning and origin (in Polish with English summary). Przegląd Geologiczny, 31: 30-36.
  • 6. Doktór, S., Graniczny, M., Kucharski, R., 1989. Astrobleme of Kościerzyna (in Polish with English summary). Przegląd Geologiczny, 37: 571-573.
  • 7. Dypvik, H., Smelror, M., Sandbakken, P., Salvigsen, O., Kaaleson, E., 2006. Traces of the marine Mjolnir impact event. Palaeogeography, Palaeoclimatology, Palaeoecology, 241: 621-636.
  • 8. French, B.M., 1998. Traces of catastrophe. A Handbook of Shock-Metamorphic Effects in Terrestrial Meteorite Impact Structures. LPI Contribution No. 954. Lunarand Planetary Institute, Houston.
  • 9. French, B.M., Koeberl, C., 2010. The convincing identification of terrestrial meteorite impact structures: what works, what doesn't, and why. Earth-Science Reviews, 98: 123-170.
  • 10. Gałązka, D., Marks, L., 2009. Geology of the Lower Vistula region, northern Poland. Polish Geological Institute Special Papers, 25: 13-20.
  • 11. Goulty, N.R., Dobson, A.J., Jones, G.D., Al.-Kindi, S.A., Holland, J.G., 2001. Gravity evidence fordiapiric ascent of the Northern Arran Granite. Journal of the Geological Society, 158: 869-876.
  • 12. Grieve, R.A.F., Pesonen, L.J., 1992. The terrestrial impact cratering record. Tectonophysics, 216: 1-30.
  • 13. Grieve, R.A.F., Pesonen, L.J., 1996. Terrestrial impact craters: Their spatial and temporal distribution and impacting bodies. Earth, Moon, Planets, 72: 357-376.
  • 14. Guterch, A., Grad, M, Thybo, H., Keller, G.R., and The POLONAISE Working Group, 1999. POLONAISE '97 - an international seismic experiment between Precambrian and Variscan Europe in Poland. Tectonophysics, 314: 101-121.
  • 15. Juhlin, C., Sturkell, E., Ebbestad, J.O.R., Lehnert, O., Hogstrom, A.E.S., Meinhold, G., 2012. A new interpretation of the sedimentary cover in the western Siljan Ring area, central Sweden, based on seismic data. Tectonophysics, 580: 88-99.
  • 16. Kenkmann, T., Poelchau, M. H., Wulf, G., 2014. Structural geology of impact craters. Journal of Structural Geology, 62: 156-182.
  • 17. Koeberl, C., 2004. Remote sensing studies of impact craters: how to be sure? Comptes Rendus Geoscience, 336: 959-961.
  • 18. Kramarska, R., Kasiński, J., Czapowski, G., Piwocki, M., Słodkowska, B., 2015. The standard section of Neogene deposits from Eastern Pomerania at Łęczyce near Lębork (northern Poland) (in Polish with English summary). Biuletyn Państwowego Instytutu Geologicznego, 461: 193-250.
  • 19. Marks, L., 2010. Timing of the Late Vistulian (Weichselian) glacial phases in Poland. Quaternary Science Reviews, 44: 81-88.
  • 20. Marzec, P., Niepsuj, M., Słonka, Ł., Pietsch, K., 2013. Application of 2-D forward seismic modeling for improved imaging of sub-salt Rotliegend strata in Polish basin. Annales Societatis Geologorum Poloniae, 83: 65-80.
  • 21. Matton, G., Jebrak, M., Lee, J.K.W., 2005. Resolving the Richat enigma: doming and hydrothermal karstification above an alkaline complex. Geology, 33: 665-668.
  • 22. Młynarski, S., 2002. Seismic refraction investigations in Poland (1964-1978) and their use in continuig studies. Geological Quarterly, 46 (3): 247-253.
  • 23. Mojski, J.E., 1973. Objaśnienia do Mapy geologicznej Polski 1:200000, ark. Grudziądz (in Polish). Wydawnictwa Geologiczne, Warszawa.
  • 24. Mojski, J.E., 1978a. Objaśnienia do Mapy geologicznej Polski 1:200 000, ark. Chojnice (in Polish). Wydawnictwa Geologiczne, Warszawa.
  • 25. Mojski, J.E., 1978b. Objaśnienia do Mapy geologicznej Polski 1:200 000, ark. Słupsk (in Polish). Wydawnictwa Geologiczne, Warszawa.
  • 26. Mojski, J.E., 1979. Objaśnienia do Mapy geologicznej Polski 1:200 000, ark. Gdańsk (in Polish). Wydawnictwa Geologiczne, Warszawa.
  • 27. Mojski, J.E., 1980. Vistulian stratigraphy in the glaciated area of the Polish Lowlands. Quaternary Studies in Poland, 2: 77-98.
  • 28. Petecki, Z., 2008. Magnetic basement in the Pomeranian segment of the Trans-European Suture Zone - NW Poland (in Polish with English summary). Prace Państwowego Instytutu Geologicznego, 191: 1-72.
  • 29. Petelski, K., 2011. The influence of sub-Qualernary basement on the relief in the eastern part of the Pomerania Lakeland, Poland. Annales Societatis Geologorum Poloniae, 81:105-114.
  • 30. Pietsch, K., Marzec, P., Niepsuj, M., Krzywiec, P., 2012. The influence of seismic velocity distribution on the depth imaging of the sub-Zechstein horizons in areas affected by salt tectonics: a case study of NW Poland. Annales Societatis Geologorum Poloniae, 82: 263-277.
  • 31. Pohl, J., Stoffler, D., Gall, H., Ernstson, K., 1977. The Ries impact structure. In: Impact and Explosion Cratering (eds. D.J. Roddy, R.O. Pepin and R.B. Merrill): 343-404. Pergamon Press, New York.
  • 32. Przybylski, B., Badura, J., 2004. May the ring structures in Sudetes have an impact origin (in Polish with English summary)? Przegląd Geologiczny, 52: 971-978.
  • 33. Reimold, W. U., 2007. The impact crater bandwagon (some problems with the terrestrial impact cratering record). Meteoritics & Planetary Science, 42: 1467-1472.
  • 34. Reimold, W.U., Ferriere, L., Deutsch, A., Koeberl, C., 2014. Impact controversies: impact recognition criteria and related issues. Meteoritics & Planetary Science, 49: 723-731.
  • 35. Riller, U., 2005. Structural characteristics of the Sudbury impact structure, Canada: impact-induced versus orogenic deformation - a review. Meteoritics & Planetary Science, 40: 1723-1740.
  • 36. Saul, J.M., 1978. Circular structures of large scale and great age on the Earth's surface. Nature, 271: 345-349.
  • 37. Schmieder, M., Jourdan, F., 2013. The Lappajarva impact structure (Finland): Age, duration of crater cooling, and implication for early life. Geochimica et Cosmochimica Acta, 112: 321-339.
  • 38. Stankowski, W. 2001. The geology and morphology of the natural reserve “Meteoryt Morasko”. Planetary and Space Science, 49: 749-753.
  • 39. Stankowski, W., Raukas, A., Bluszcz, A., Fedorowicz, S., 2007. Luminescence dating of the Morasko (Poland), Kaali, Ilumetsa and Tsoorikmae (Estonia) meteorite craters. Geochronometria, 28: 25-29.
  • 40. Stewart, S.A., Allen, P.J., 2002. A 20-km-diameter multi-ringed impact structure in the North Sea. Nature, 418: 520-523.
  • 41. Stoffler, D., Artemieva, N.A., Pierazzo, F., Ivanov, B.A., 2001. Ries crater, Germany: geology and numerical modeling of impact cratering. Meteoritics & Planetary Science, 36 (9): Supplement, A199.
  • 42. Suuroja, K., Suuroja, S., 2010. The Neugrand meteorite crater on the seafloor of the Gulf of Finland, Estonia. Baltica, 23: 47-58.
  • 43. Taud, H., Parrot, J.-F., 1992. Detection of circular structures on satellite images. International Journal of Remote Sensing, 13: 319-335.
  • 44. Turtle, E. P., Pierazzo, E., 1998. Constraints on the size of the Vredefort impact crater from numerical modeling. Meteoritics & Planetary Science, 33: 483-490.
  • 45. Uścinowicz, G., 2014. Impact craters and the extraterrestrial matter in their surroundings: case of Morasko (Poland) and Kaali (Estonia). Baltica, 27: 24-31.
  • 46. Znosko, J., Dadlez, R., Grocholewski, A., Kowalczewski, Z., Ryłko, W., Ryka, W., 1998. Tectonic map of Poland, 1:500 000. In: Tectonic Atlas of Poland (ed. J. Znosko). Polish Geological Institute, Warszawa.
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-dcf03f6f-8040-472f-af35-ddd2c1cf6114
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