PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Heavy minerals as a tool to reconstruct river activity during the Weichselian glaciation (Toruń Basin, Poland)

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The heavy-mineral composition of the Weichselian fluvial successions deposited by an ephemeral meandering river and by a sand-bed braided river in the Toruń Basin (central Poland) was analysed. On the basis of a lithofacies analysis, in combination with the composition of the heavy-mineral assemblages, the fluvial processes and river-channel morphology were reconstructed. This allows determining the provenance of the fluvial deposits and the rivers’ discharge regimes. A model is proposed which can explain the changes in the amount of individual minerals in the fluvial sediments of different ages under the conditions of the oscillating Scandinavian ice sheet. The model assumes that, during the ice-sheet advances, the proglacial streams supplied large amounts of heavy minerals that were less resistant to mechanical abrasion. During the main phase of the ice-sheet retreat, the distance between the ice sheet and the Toruń Basin increased, and the amount of non-resistant minerals diminished as a result of sediment reworking in proglacial rivers. Due to the unique location of the Toruń Basin at the front of the Scandinavian ice sheet during the Weichselian glaciation, the heavy-mineral assemblages in the fluvial deposits form a valuable tool for the recognition of the ice-sheet extent.
Czasopismo
Rocznik
Strony
25--46
Opis fizyczny
Bibliogr. 80 poz.
Twórcy
  • Faculty of Earth Sciences, Nicolaus Copernicus University, Lwowska 1, 87-100 Toruń, Poland
  • Faculty of Earth Sciences, Nicolaus Copernicus University, Lwowska 1, 87-100 Toruń, Poland
Bibliografia
  • Alexander, J., Bridge, J.S., Cheelà, R.J. & Leclair, S.F., 2001. Bedforms and associated sedimentary structures formed under supercritical water flows over aggrading sand beds. Sedimentology 48, 133-152.
  • Ashworth, P.J., Best, J.L., Roden, J.E., Bristow, C.S. & Klaassen, G.J., 2000. Morphological evolution and dynamics of a large, sand braid-bar, Jamuna River, Bangladesh. Sedimentology 47, 533-555.
  • Ashworth, P.J., Sambrook Smith, G.H., Best, J.L., Bridge, J.S., Lane, S.N., Lunt, I.A., Reesink, A.J.H., Simpson, C.J. & Thomas, R.E., 2011. Evolution and sedimentology of a channel fill in the sandy braided South Saskatchewan River and its comparison to the deposits of an adjacent compound bar. Sedimentology 58, 1860-1883.
  • Bateman, R.M. & Cat, J.A., 2007. Provenance and palaeoenvironmental interpretation of superficial deposits, with Particular reference to post-depositional modification of heavy mineral assemblages. [In:] M.A. Mange & D.T. Wright (Eds): Heavy minerals in use. Developments in Sedimentology 58, 151-188.
  • Bridge, J.S., 1993. The interaction between channel geometry, water flow, sediment transport and deposition in braided rivers. [In:] J.L. Best & C.S. Bristow (Eds): Braided rivers. Geological Society Special Publication 75, 13-71.
  • Bridge, J.S., 2003. Rivers and floodplains: forms, processes, and sedimentary record. Blackwell Publishing, Oxford, 504 pp.
  • Brykczyński, M., 1986. O głównych kierunkach rozwoju sieci rzecznej Niżu Polskiego w czwartorzędzie [On the main directions of the development of the Polish lowland river network in the Quaternary]. Przegląd Geograficzny 58, 411-440.
  • Busschers, F.S., Weerts, H.J.T., Wallinga, J., Kasse, C., Cleveringa, P., De Wolf, H. & Cohen, K.M., 2005. Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits - fluvial response to climate change, sea-level fluctuation and glaciation. Netherlands Journal of Geosciences 84, 25-41.
  • Cant, D.J. & Walker, R.G., 1978. Fluvial processes and facies sequences in the sandy braided South Saskatchewan River, Canada. Sedimentology 25, 625-648.
  • Church, M., 1988. Floods in cold climates. [In:] V.R. Baker, R.C. Kochel & P.C. Patton (Eds): Flood Geomorphology. Wiley, New York, 205-231.
  • Clemens, K.E. & Komar, P.D., 1988. Oregon beach sand compositions produced by the mixing of sediments under a transgressing sea. Journal of Sedimentary Petrology 58, 519-529.
  • Cordier, S., Harmand, D., Frechen, M. & Beiner, M., 2006. Fluvial system response to Middle and Upper Pleistocene climate change in the Meurthe and Moselle valleys (Eastern Paris Basin and Rhenish Massif). Quaternary Science Reviews 25, 1460-1474.
  • Eyles, N., Eyles, C.H. & Miall, A.D., 1983. Lithofacies types and vertical profile models; an alternative approach to the description and environmental interpretation of glacial diamict and diamictite sequences. Sedimentology 30, 393-410.
  • Fletcher, W.K., Church, M. & Wolcott, J., 1992. Fluvial-transport equivalence of heavy minerals in the sand size range. Canadian Journal of Earth Sciences 29, 2017-2021.
  • Folk, R.L. & Ward, W.C., 1957. Brazos River bar: a study in the significance of grain size parameters. Journal of Sedimentary Petrology 27, 3-26.
  • Galon, R., 1961. Morphology of the Noteć-Warta (or Toruń-Eberswalde) ice marginal streamway. Prace Geograficzne IGiPZ PAN 29, 1-129.
  • Galon, R., 1968. New facts and problems pertaining to the origin of the Noteć Warta Pradolina and the valleys linked with it. Przegląd Geograficzny 40, 307-315.
  • Gorrell, G. & Shaw, J., 1991. Deposition in an esker, bead and fan complex, Lenark, Ontario, Canada. Sedimentary Geology 72, 285-314.
  • Górska, M., 2006. Wybrane cechy teksturalne glin lodowcowych i osadów wodnolodowcowych fazy pomorskiej pólnocno-wschodnich Niemiec [Some textural features of till and fluvioglacial deposits of the Pomeranian Phase in north-eastern Germany]. Przegląd Geograficzny 78, 69-89.
  • Haldorsen, S., Jørgensen, P., Rappol, M. & Riezebos, P.A., 1989. Composition and source of the clay-sized fraction of Saalian till in The Netherlands. Boreas 18, 89-97.
  • Huisink, M., 2000. Changing river styles in response to Weichselian climate changes in the Vecht valley, eastern Netherlands. Sedimentary Geology 133, 115-134.
  • Kasse, C., Bohncke, S. & Vandenberghe, J., 1995. Fluvial periglacial environments, climate and vegetation during the Middle Weichselian with special reference to the Hengelo Interstadial. Mededelingen Rijks Geologische Dienst 52, 387-413.
  • Kasse, C., Vandenberghe, J., De Corte, F. & van den Haute, P., 2007. Late Weichselian fluvio-aeolian sands and coversands of the type locality Grubbenvorst (southern Netherlands): sedimentary environments, climate record and age. Journal of Quaternary Sciences 22, 695-708.
  • Kasse, C., Vandenberghe, J., van Huissteden, J., Bohncke, S.J.P. & Bos, J.A.A., 2003. Sensitivity of Weichselian fluvial systems to climate change (Nochten mine, eastern Germany). Quaternary Sciences Review 22, 2141-2156.
  • Kenig, K., Jochemczyk, L. & Trzepla, M., 2006. Litogeneza piaszczystych osadów międzymorenowych w środkowej części Pojezierza Chełmińskiego [Lithogenesis of intertill sand deposits from the central part of the Chełmno Lakeland]. Przegląd Geologiczny 54, 807-814.
  • Komar, P.D., 2007. The entrainment, transport and sorting of heavy minerals by waves and currents. [In:] M.A. Mange & D.T. Wright (Eds): Heavy minerals in use. Developments in Sedimentology 58, 3-48.
  • Kozarski, S., 1988. Origin of pradolinas: a discussion of mistaken ideas. Zeitschrift für Gletscherkunde und Glazialgeologie 24, 75-92.
  • Krzyszkowski, D., 1990. Middle and late Weichselian stratigraphy and palaeoenvironments in central Poland. Boreas 19, 333-350.
  • Krzyszkowski, D., 1995. An outline of the Pleistocene stratigraphy of the Kleszczów Graben (Bełchatów outcrop), central Poland. Quaternary Science Reviews 14, 61-83.
  • Krzyszkowski, D., 1996. Climatic control on Quaternary fluvial sedimentation in the Kleszczów Graben, central Poland. Quaternary Science Reviews 15, 315-333.
  • Lee, J.R., Rose, J., Hamblin, R.J.O. & Moorlock, B.S.P., 2004. Dating the earliest lowland glaciation of eastern England: a pre-MIS 12 early Middle Pleistocene Happisburgh Formation glaciation. Quaternary Science Reviews 23: 1551-1566.
  • Lindner, L., Lamparski, Z. & Dąbrowski, S., 1982. River valleys of Mazovian interglacial in eastern Central Europe. Acta Geologica Polonica 32, 179-190.
  • Lowright, R., Williams, E.G. & Dachille, F., 1972. An analysis of factors controlling deviations in hydraulic equivalence in some modern sands. Journal of Sedimentary Petrology 44, 635-645.
  • Ludwikowska-Kędzia, M., 2013. The composition of transparent heavy minerals in Quaternary sediments of the Kielce-Łagów valley (Holy Cross Mountains, Poland). Geologos 19 (this issue), 95-129.
  • Makowska, A., 1979. Interglacjał eemski w Dolinie Dolnej Wisły [Eemian interglacial in valley of lower Vistula River]. Studia Geologica Polonica 63, 1-90.
  • Makowska, A., 1980. Late Eemian with preglacial and glacial part of Vistulian Glaciation in Lower Vistula Region. Quaternary Studies in Poland 2, 37-56.
  • Mange, M.A. & Maurer, H.F.W., 1992. Heavy minerals in colour. Chapman and Hall, London, 147 pp.
  • Marcinkowski, B., 2007. Wykorzystanie składu mineralnego i morfologii ziaren minerałów ciężkich do określania środowiska sedymentacyjnego [Application of the mineral content and grain morphology of heavy minerals to interpret the sedimentary environment]. Przegląd Geologiczny 55, 1-207.
  • Marcinkowski, B. & Mycielska-Dowgiałło, E., 2013. Heavy-mineral analysis in Polish investigations of Quaternary deposits: a review. Geologos 19 (this issue), 5-23.
  • Miall, A.D., 1978. Lithofacies types and vertical profile models in braided rivers: a summary. [In:] A.D. Miall (Ed.): Fluvial Sedimentology. Canadian Society of Petroleum Geologists, Memoir 5, 597-604.
  • Miall, A.D., 2006. The geology of fluvial deposits. Sedimentary facies, basin analysis, and petroleum geology. Springer, Berlin, 598 pp.
  • Mol, J., Vandenberghe, J. & Kasse, C., 2000. River response to variations of periglacial climate in mid-latitude Europe. Geomorphology 33, 131-148.
  • Mol, J., 1997. Fluvial response to Weichselian climate changes in the Niederlausitz (Germany). Journal of Quaternary Science 12, 43-60.
  • Molewski, P., 2007. Neotektoniczne i glacidynamiczne uwarunkowania wykształcenia plejstocenu Wysoczyzny Kujawskiej [Neotectonic and glacidynamic conditions of the formation of the Pleistocene of the Kujawy moraine plateau]. Nicolas Copernicus University, Toruń, 139 pp.
  • Morton, A.C. & Hallsworth, C.R., 1999. Processes controlling the composition of heavy mineral assemblages in sandstones. Sedimentary Geology 124, 3-29.
  • Morton, A., Hounslow, M.W. & Frei, D., 2013. Heavy-mineral, mineral-chemical and zircon-age constraints on the provenance of Triassic sandstones from the Devon coast, southern Britain. Geologos 19 (this issue), 67-85.
  • Niewiarowski, W., 1968. Morfologia i rozwój pradoliny i doliny dolnej Drwęcy [Morphology and evolution of the pradolina and valley of the Drwęca River]. Studia Societatis Scientiarum Torunensis 6, 132 pp.
  • Niewiarowski, W., 1969. The relation of the Drwęca valley to the Noteć-Warta (Toruń-Eberswalde) Pradolina and its role in the glacial and lateglacial drainage system. Geographia Polonica 17, 173-188.
  • Popp, S., Belolyubsky, I., Lehmkuhl, F., Prokopiev, A., Siegert, C., Spektor, V., Stauch, G. & Diekmann, B., 2007. Sediment provenance of Late Quaternary morainic, fluvial and loess-like deposits in the southwestern Verkhoyansk Mountains (eastern Siberia) and implications for regional palaeoenvironmental reconstructions. Geological Journal 42, 477-497.
  • Racinowski, R., 1995. Analiza minerałów ciężkich w badaniach osadów czwartorzędowych Polski [Remarks on the use of results of heavy-mineral analysis for studies on Quaternary sediments of Poland]. [In:] E. Mycielska-Dowgiałło & J. Rutkowski (Eds): Badania osadów czwartorzędowych. Wybrane metody i interpretacja wyników [Investigation of Quaternary sediments. Some methods and interpretation of the results]. WGiSR UW, Warszawa, 151-166.
  • Racinowski, R., 2000. Niektóre problemy interpretacji wyników analiz minerałów ciężkich w badaniach osadów czwartorzędowych [Some aspects of the interpretation of the results of heavy-mineral analyses in the research of Quaternary deposits]. Przegląd Geologiczny 48, 354-359.
  • Racinowski, R., 2010. Główne przezroczyste minerały ciężkie w osadach czwartorzędowych Polski [Main transparent heavy minerals in Quaternary deposits]. Biuletyn PIG 438, 99-106.
  • Rappol, M. & Stoltenberg, H.M.P., 1985. Compositional variability of Saalien till in The Netherlands and its origin. Boreas 14, 33-50.
  • Russell, H.A.J., Sharpe, D.R. & Bajc, A.F., 2007. Sedimentary signatures of the Waterloo Moraine, Ontario, Canada. [In:] M.J. Hambrey, P. Christoffersen, N.F. Glasser & B. Hubbard (Eds): Glacial sedimentary processes and products. International Association of Sedimentologists Special Publication 39, 85-108.
  • Sambrook Smith, G.H., Ashworth, P.J., Best, J.L., Woodward, J. & Simpson C.J., 2006. The sedimentology and alluvial architecture of the sandy braided South Saskatchewan River, Canada. Sedimentology 53, 413-434.
  • Toucanne, S., Zaragosi, S., Bourillet, J.F., Gibbard, P.L., Eynaud, F., Giraudeau, J., Turon, J.L., Cremer, M., Cortijo, E., Martinez, P. & Rossignol, L., 2009. A 1.2 Ma record of glaciation and fluvial discharge from the West European Atlantic margin. Quaternary Science Reviews 28, 2974-2981.
  • Van Huissteden, J., 1990. Tundra rivers of the Last Glacial: sedimentation and geomorphological processes during the middle Pleniglacial in Twente, Eastern Netherlands. Mededelingen Rijks Geologische Dienst 44, 3-138.
  • Van Huissteden, J., Gibbard, P.L. & Briant, R.M., 2001. Periglacial fluvial systems in northwest Europe during marine isotope stages 4 and 3. Quaternary International 79, 75-88.
  • Van Huissteden, J. & Kasse, C., 2001. Detection of rapid climate change in Last Glacial fluvial successions in The Netherlands. Global and Planetary Change 28, 319-339.
  • Vandenberghe, J., 1995. Timescales, climate and river development. Quaternary Science Reviews 14, 631-638.
  • Vandenberghe, J., 2001. A typology of Pleistocene cold-based rivers. Quaternary International 79, 111-121.
  • Vandenberghe, J., 2002. The relation between climate and river processes, landforms and deposits during the Quaternary. Quaternary International 91, 17-23.
  • Vandenberghe, J., 2003. Climate forcing of fluvial system development: an evolution of ideas. Quaternary Science Reviews 22, 2053-2060.
  • Wachecka-Kotkowska, L. & Ludwikowska-Kędzia, M., 2013. Heavy-mineral assemblages from fluvial Pleniglacial deposits of the Piotrków Plateau and the Holy Cross Mountains - a comparative study. Geologos 19 (this issue), 131-146.
  • Weckwerth, P., 2009. Środowisko depozycji fluwialnej w stadiale głównym zlodowacenia Wisły - stanowisko Nowe Dąbie, południowo-zachodnia część Kotliny Toruńskiej [Fluvial depositional environment of the main stadial of the Weichselian glaciation - Nowe Dąbie pit, SW part of the Toruń Basin]. [In:] M. Pisarska-Jamroży & Z. Babiński (Eds): Plejstoceńskie środowiska sedymentacyjne Pojezierza Pomorskiego [Pleistocene sedimentary environments of Pomeranian Lakeland]. Wydawnictwo UKW, Bydgoszcz, 90-99.
  • Weckwerth, P., 2010. Evolution of the Toruń Basin in the Late Weichselian. Landform Analysis 14, 57-84.
  • Weckwerth, P., 2011. Palaeoslopes of Weichselian sand-bed braided rivers in the Toruń Basin (Poland): results of palaeohydraulic analysis. Geologos 17, 227-238.
  • Weckwerth, P., 2013. Procesy fluwialne toruńskiego basenu sedymentacyjnego podczas zlodowacenia wisły [Fluvial processes of the Toruń sedimentary basin during the Weichselian glaciation]. Nicolaus Copernicus University, Toruń (in press).
  • Weckwerth, P., Przegiętka, K., Chruścińska, A. & Pisarska-Jamroży, M., 2013. The relation between optical bleaching and sedimentological features of fluvial deposits in the Toruń Basin (Poland). Geological Quarterly 57, 31-44.
  • Weckwerth, P., Przegiętka, K., Chruścińska, A., Woronko, B. & Oczkowski, H.L., 2011. Age and sedimentological features of fluvial series in the Toruń Basin and the Drwęca valley (Poland). Geochronometria 38, 397-412.
  • Wentworth, C.K., 1922. A scale of grade and class terms for clastic sediments. Journal of Geology 30, 377-392.
  • Westaway, R. & Bridgland, D., 2010. Causes, consequences and chronology of large-magnitude palaeoflows in Middle and Late Pleistocene river systems of northwest Europe. Earth Surface Processes and Landforms 35, 1071-1094.
  • Woronko, B., Rychel, J., Karasiewicz, M.T., Ber, A., Krzywicki, T., Marks, L. & Pochocka-Szwarc, K., 2013. Heavy and light minerals as a tool for reconstruction of depositional environments: an example from the Jałówka site (northern Podlasie region, NE Poland). Geologos 19 (this issue), 47-66.
  • Wysota, W., 2002. Stratygrafia i środowiska sedymentacji zlodowacenia wisły w południowej części dolnego Powiśla [Stratigraphy and sedimentary environments of the Weichselian glaciation in the southern part of the Lower Vistula region]. Nicolas Copernicus University, Toruń, 144 pp.
  • Wysota W., Lankuaf, K.R., Molewski, P. & Szmańda, J., 1996. Sedymentologia interstadialnej serii rzecznej (Rzęczkowo) zlodowacenia Wisły (Vistulian) odsłoniętej w SW krawędzi Wysoczyzny Chemińskiej [Sedimentology of the interstadial fluvial succession (Rzęczkowo) of the Vistulian glaciations exposed in the SW margin of the Chełmno moraine plateau]. Acta Universitatis Nicolai Copernici, Geografia 28, 39-63.
  • Wysota, W., Molewski, P. & Sokołowski, R.J., 2009. Record of the Vistula ice lobe advances in the Late Weichselian glacial sequence in north-central Poland. Quaternary International 207, 26-41.
  • Zieliński, T., 1995. Kod litofacjalny i litogenetyczny - konstrukcja i zastosowanie [Lithofacies and genetic codes: construction and application]. [In:] E. Mycielska-Dowgiałło & J. Rutkowski (Eds): Badania osadów czwartorzędowych [Investigation of Quaternary sediments]. Warsaw University Press, Warszawa, 220-235.
  • Zieliński, T., 1998. Litofacjalna identyfikacja osadów rzecznych [Lithofacies identification of alluvial sediments]. [In:] E. Mycielska-Dowgiałło (Ed.): Struktury sedymentacyjne i postsedymentacyjne w osadach czwartorzędowych i ich wartość interpretacyjna [Sedimentary and postsedimentary structures in Quaternary sediments and their significance for interpretations]. Warsaw University Press, Warszawa, 195-257.
  • Zieliński, T., 2007. The Pleistocene climate-controlled fluvial sedimentary record in the Bełchatów mine (central Poland). Sedimentary Geology 193, 203-209.
  • Zieliński, T. & Pisarska-Jamroży, M., 2012. Jakie cechy litologiczne warto kodować, a jakie nie? [Which features of deposits should be included in a code and which not?]. Przegląd Geologiczny 60, 387-397.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-34f8ca9e-515c-4778-8038-185962eabb22
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.