Skip to main content
Have a personal or library account? Click to login
Is the Charlottenthal fan (marginal zone of the Pomeranian phase, NE Germany) an end moraine? Cover

Is the Charlottenthal fan (marginal zone of the Pomeranian phase, NE Germany) an end moraine?

Geologos
Volume 17 (2011): Issue 1 (April 2011)
By:  and    
Open Access
|Apr 2011
References

References

  1. Bartkowski, T., 1972. Internal structure of marginal zone forms in the area of last glaciation in the Polish Lowland.13, 27-67.
    Search in Google Scholar
  2. Blair, T. C. & McPherson, J. G., 1994. Alluvial fans and their natural distinction from rivers based on morphology, hydraulic processes, sedimentary processes, and their facies assemblages.A64, 450-489.
    Open DOISearch in Google Scholar
  3. Börner, A. & Müller, U., 2009.[Report on the lithostratigraphical positioning of tills from the ‘Charlottenthal gravel pit’]. Unpublished report, LUNG M-V, Güstrow, 6 pp.
    Search in Google Scholar
  4. Bremer, F., 2000.LUNG M-V, Güstrow.
    Search in Google Scholar
  5. Dobracki, R. & Krzyszkowski, D., 1997. Sedimentation and erosion at the Weichselian ice marginal zone near Golczewo, NW Poland.16, 721-740.
    Open DOISearch in Google Scholar
  6. Flint, R. F. 1971.Wiley, New York, 589 pp.
    Search in Google Scholar
  7. GFE, 2000.3 [Report on the exploration of quartz and quartzite in owned-property resources in Charlottenthal 3]. Unpublished report, GKM GmbH, Schwerin, 7 Appendices, 16 pp.
    Search in Google Scholar
  8. Górska-Zabielska, M. & Pisarska-Jamroży, M., 2008. Zróżnicowanie petrograficzne plejstoceńskich osadów Pojezierza Myśliborskiego na przykładzie żwiórw z Chełma Górnego i Cedyni [Petrographical differentiation of Pleistocene deposits of the Myślibórz Lakeland (Western Pomerania) based on gravels from Chełm Górny and Cedynia].56, 317-321.
    Search in Google Scholar
  9. Górska-Zabielska, M., 2008. Fennoskandzkie obszary alimentacyjne osadów akumulacji glacjalnej i glacjofluwialnej lobu Odry [Fennoscandinavian source areas of the glacial and glaciofluvial deposits of the Odra lobe].78, 330 pp.
    Search in Google Scholar
  10. Harms, J. C., Southard, J. B. & Walker, R. G., 1982.Short course No. 9 lecture notes, SEPM, Tulsa, 250 pp.
    Open DOISearch in Google Scholar
  11. Harvey, A. M., 1984. Debris flow and fluvial deposits in Spanish Quaternary alluvial fans: implications for fan morphology. [In:] E. H. Koster & R. J. Steel (Eds):Canadian Society of Petroleum Geologists Memoir 10, 123-132.
    Search in Google Scholar
  12. Instrukcja, 1996. Instrukcja opracowania i wydania Szczegółowej Mapy Geologicznej Polski w skali 1:50 000 [Instruction for preparation and edition of the Detailed Geological Map of Poland at scale 1:50,000]. PIG Press, Warszawa.
    Search in Google Scholar
  13. Johnson, A. M. & Rodine, J. R., 1984. Debris flow. [In:] D. Brundsen & D. B. Prior (Eds):Wiley, Chichester, 257-361.
    Search in Google Scholar
  14. Kasprzak, L., 1988. Dyferencjacja mechanizmów formowania stref marginalnych faz leszczyńskiej i poznańskiej ostatniego zlodowacenia na Nizinie Wielkopolskiej [Differentiation of the mechanisms involved in the formation of the marginal zones of the Leszno and Poznań phases of the last glaciation, Great Polish Lowland].5/6, 159 pp.
    Search in Google Scholar
  15. Krüger, J. & Kjær, K. H., 1999. A data chart for field description and genetic interpretation of glacial diamicts and associated sediments with examples from Greenland, Iceland, and Denmark.28, 386-402.
    Open DOISearch in Google Scholar
  16. Krzyszkowski, D. & Zieliński, T., 2002. The Pleistocene end moraine fans: controls on their sedimentation and location.149, 73-92.
    Open DOISearch in Google Scholar
  17. Lüttig, G., 1958. Methodische Fragen der Geschiebeforschung [Questions on the methodology of the analysis of erratics].75, 361-418.
    Search in Google Scholar
  18. McKee, E. D., Crosby, E. J. & Berryhill, H. L., 1967. Flood deposits, Bijou Creek, Colorado.37, 829-851.
    Open DOISearch in Google Scholar
  19. Miall, A. D., 1977. A review of the braided river depositional environment.13, 1-62.
    Open DOISearch in Google Scholar
  20. Miall, A. D., 1978. Lithofacies types and vertical profile models in braided river deposits: a summary. [In:] A. D. Miall (Ed.):Canadian Society of Petroleum Geologists Memoir 5, 597-604.
    Search in Google Scholar
  21. Miall, A. D., 1985. Architectural element analysis: a new method of facies analysis applied to fluvial deposits.22, 261-308.
    Open DOISearch in Google Scholar
  22. Mohrig, D., Heller, P. L., Paola, C. & Lyons, W. J., 2000. Interpreting avulsion process from ancient alluvial sequences: Guadalope-Matarranya system (northern Spain) and Wasatch Formation (western Colorado).112, 1787-1803.
    Open DOISearch in Google Scholar
  23. Nemec, W. & Steel, R. J., 1984. Alluvial and coastal conglomerates: their significant features and some comments on gravelly mass-flow deposits. [In:] E. H. Koster & R. J. Steel (Eds):Canadian Society of Petroleum Geologists Memoir 10, 1-31.
    Search in Google Scholar
  24. Nemec, W., 1990. Aspects of sediment movement on steep delta slope. [In:] A. Colella & D. B. Prior (Eds):International Association of Sedimentologists Special Publication 10, 29-73.
    Open DOISearch in Google Scholar
  25. Pisarska-Jamroży, M., 2006. Transitional deposits between end moraine and sandur plain in the Pomeranian glacimarginal zone of NW Poland: a missing component of ice-contact sedimentary models.35, 126-141.
    Open DOISearch in Google Scholar
  26. Pisarska-Jamroży, M., 2008. Zonation of glaciomarginal environment inferred from Pleistocene deposits of Myślibórz Lakeland, NW Poland.90A, 237-249.
    Open DOISearch in Google Scholar
  27. Rühberg, N., Schulz, W., Von Bülow, W., Müller, U., Krienke, H. D., Bremer, F. & Dann, T., 1995. V. Mecklenburg-Vorpommern. [In:] L. Benda (Ed.):Berlin, 95-115.
    Search in Google Scholar
  28. Ruszczyńska-Szenajch, H., 1982. Depositional processes of Pleistocene lowland end moraines, and their possible relation to climatic conditions.11, 250-260.
    Open DOISearch in Google Scholar
  29. Schulz, W., 1962.[Report on the general geological mapping 1:100 000: Sheet 2339 - Krakow, with geological map 1:25 000]. Unpublished report, VEB Geologische Erkundung Nord (GFE), Schwerin.
    Search in Google Scholar
  30. Schulz, W., 1963. Eisrandlagen und Seeterrassen in der Umgebung von Krakow am See in Mecklenburg.12, 1152-1168.
    Search in Google Scholar
  31. Schulz, W., 1996. Zur Bedeutung der Korngröße bei Geschiebezählungen.29, 91-102.
    Search in Google Scholar
  32. Scott, K. M., 1971. Origin and sedimentology of 1969 debris flow near Glendora, California.750-C, 242-247.
    Search in Google Scholar
  33. Sharp, R. P. & Nobles, L. H., 1953. Mudflow of 1941 at Wrightwood, Southern California.64, 547-560.
    Open DOISearch in Google Scholar
  34. Smith, N. D., 1970. The braided stream depositional environments: comparison of the Platte River with some Silurian clastic rocks, north-central Appalachians.81, 2993-3014.
    Open DOISearch in Google Scholar
  35. TGL 25232, 1980.[Analysis of the clast content of Quaternary tills]. Zentrales Geologisches Institut, Berlin, 35 pp.
    Search in Google Scholar
  36. Woldstedt, P. 1961.1. F. Enke, Stuttgart, 374 pp.
    Search in Google Scholar
  37. Zieliński, T. & Van Loon, A. J., 1996. Characteristics and genesis of moraine-derived flow till varieties.101, 119-143.
    Open DOISearch in Google Scholar
  38. Zieliński, T., 1992.[Marginal moraines of NE Poland - sediments and depositional conditions]. Silesian University, Katowice, 95 pp.
    Search in Google Scholar
  39. Zieliński, T., 1993.[Outwash plains of NE Poland - sediments and depositional processes]. Silesian University, Katowice, 96 pp.
    Search in Google Scholar
  40. Zieliński, T., 2003. Czy możliwa jest identyfkacja środowiska glacimarginalnego na podstawie kryterium litologicznego? [Is lithology a useful tool for the recognition of the glaciomarginal environment?] [In:] M. Harasimiuk & S. Terpiłowski (Eds):[Sedimentological analysis of glaciogenic sediments]. UMCS Press, Lublin, 95-104.
    Search in Google Scholar
DOI: https://doi.org/10.2478/v10118-011-0002-9 | Journal eISSN: 2080-6574 | Journal ISSN: 1426-8981
Journal RSS Feed
Language: English
Page range: 17 - 28
Published on: Apr 4, 2011
Published by: Adam Mickiewicz University
In partnership with: Paradigm Publishing Services
Keywords:
transitional fan,
glaciofluvial sediments,
gravel petrography,
Weichselian glaciation,
Pomeranian Phase,
NE Germany
Related subjects:
Geosciences,
Geology and mineralogy

© 2011 Małgorzata Pisarska-Jamroży, Andreas Börner, published by Adam Mickiewicz University
This work is licensed under the Creative Commons License.

Volume 17 (2011): Issue 1 (April 2011)
Previous article
Next article