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Neotectonic evolution and sediment budget of the Meuse catchment in the Ardennes and the Roer Valley Rift System

Published online by Cambridge University Press:  01 April 2016

R.T. Van Balen ,
R.F. Houtgast ,
F.M. Van der Wateren  and
J. Vandenberghe
R.T. Van Balen*
Affiliation:
Vrije Universiteit, Faculteit der Aard- en Levenswetenschappen, de Boelelaan 1085, Amsterdam, the Netherlands; e-mail: balr@geo.vu.nl
R.F. Houtgast
Affiliation:
Vrije Universiteit, Faculteit der Aard- en Levenswetenschappen, de Boelelaan 1085, Amsterdam, the Netherlands; e-mail: balr@geo.vu.nl
F.M. Van der Wateren
Affiliation:
Vrije Universiteit, Faculteit der Aard- en Levenswetenschappen, de Boelelaan 1085, Amsterdam, the Netherlands; e-mail: balr@geo.vu.nl
J. Vandenberghe
Affiliation:
Vrije Universiteit, Faculteit der Aard- en Levenswetenschappen, de Boelelaan 1085, Amsterdam, the Netherlands; e-mail: balr@geo.vu.nl
*
1corresponding author
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Abstract

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Using marine planation surfaces, fluvial terraces and a digital terrain model, the amount of eroded rock volume versus time for the Meuse catchment has been computed. A comparison of the amount of eroded volume with the volume of sediment preserved in the Roer Valley Rift System shows that 12% of the eroded volume is trapped in this rift. The neotectonic uplift evolution of the Ardennes is inferred from the incision history of the Meuse River system and compared to the subsidence characteristics of the Roer Valley Rift System. Both areas are characterized by an early Middle Pleistocene uplift event.

Keywords

MeuseRoer Valley Grabenneotectonicsriver terracesArdennessediment budget
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 81 , Special Issue 2: Rift tectonics and syngenetic sedimentation - the Cenozoic Lower Rhine Basin and related structures , August 2002 , pp. 211 - 215
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2002

References

Ahorner, L., Van Gils, J.M., Flick, J., Houtgast, G. & Ritsema, A.R., 1976. First draft of the earthquake zoning map of NW Germany, Belgium, Luxembourg and the Netherlands. Kon. Ned. Met. Inst. De Bilt 153: 39–41.Google Scholar
Camelbeeck, T. & Meghraoui, M., 1998. Geological and geophysical evidence for large palaeo-earthquakes with surface faulting in the Roer Graben (northwest Europe). Geophysical Journal International 132: 347–362.Google Scholar
Cornet, Y., 1995. L’encaissement de rivières ardennaises au cours du Quaternaire. In: Demoulin, A. (ed.): L’Ardenne, essai de gèografie physique. Dep. Géogr. Phys. Quat., Univ. Liège: 155–177.Google Scholar
Demoulin, A., 1995a. L’Ardenne des Plateaux, heritage des temps anciens - sufaces d’érosion en Arderme. In: Demoulin, A. (ed.): L’Ardenne, essai de géografie physique. Dep. Géogr. Phys. Quat., Univ. Liège: 68–93.Google Scholar
Demoulin, A., 1995b. L’Ardenne bouge toujours - neotectonique du massif Ardennais. In: Demoulin, A. (ed.): L’Ardenne, essai de géografie physique. Dep. Géogr. Phys. Quat., Univ. Liège: 110–135.Google Scholar
Garcia-Castellanos, D., Cloetingh, S. & Van Balen, R.T., 2000. Modelling the middle Pleistocene uplift in the Ardennes-Rhenish Massif: thermo-mechanical weakening under the Eifel? Global and Planetary Change 27: 39–52 Google Scholar
Geluk, M.C., Duin, E.J.Th., Rijkers, R.H.B., Van den Berg, M.W. & Van Rooijen, P., 1994. Stratigraphy and tectonics of the Roer Valley Graben. Geologie en Mijnbouw 73: 129–141.Google Scholar
Grimbérieux, J., Laurant, A. & Ozer, P., 1995. Les rivières s’installent. In: Demoulin, A. (ed.): L’Ardenne, essai de géografie physique. Dep. Géogr. Phys. Quat., Univ. Liège: 94–109.Google Scholar
Haq, B.U., Hardenbol, J. & Vail, P., 1987. Chronology of fluctuating sea levels since theTriassic. Science 235: 1156–1167.Google Scholar
Hoselmann, C. 1996. Der Haupterrassen-Komplex am unteren Mittelrhein. Zeitschrift Deutsche Geologische Geselschaft 147: 481–497.Google Scholar
Houtgast, G., 1992. Catalogus van aardbevingen in Nederland t/m 1990. Koninklijk Nederlands Meteorologisch Instituut. De Bilt 179: 166 pp.Google Scholar
Houtgast, R.F. & Van Balen, R.T., 2000. Neotectonics of the Roer Valley Rift System, the Netherlands. Global and Planetary Change 27: 131–146.Google Scholar
Juvigné, E. & Renard, F., 1992. Les terrasses de la Meuse de Liège à Maastricht. Annales société géologique de Belgique 115: 167–186.Google Scholar
Meyer, W. & Stets, J., 1998. Junge Tektonik im Rheinischen Schiefergebirge und ihre Quantifizierung. Zeitschrift Deutsche Geologische Geselschaft 149: 359–379.CrossRefGoogle Scholar
Paulissen, E., Vandenberghe, J., & Gullentops, F., 1985. The Feldbiss fault in the Maas Valley bottom (Limburg, Belgium). Geologie en Mijnbouw 64: 79–87.Google Scholar
Pissart, A., 1974. La Meuse en France et en Belgique. Formation du basin hydrographique. Les terrasses et leur enseignements, In: Macar, P. (ed.): L’évolution quaternaire des basins fluviaux de la mer du nord mérondiale. Centenaire de la société géologique de Belgique, Liège: 105–131.Google Scholar
Pissart, A., Harmand, D. & Krook, L., 1997. L’évolution de la Meuse de Toul à Maastricht depuis le Miocène: corrélations chronologiques et traces des capturesde la Meuse Lorraine d’après les minéraux denses. Géographie physique et Quaternaire 51: 267–284.Google Scholar
Van Balen, R.T., Houtgast, R.F., Van der Wateren, F.M., Vandenberghe, J. & Bogaart, P.W. 2000. Sediment budget and tectonic evolution of the Meuse catchment in the Ardennes and the Roer Valley Rift System. Global and Planetary Change 27: 113–129.Google Scholar
Van Eck, T. & Davenport, C.A., 1994. Seismotectonics and seismic hazard in the Roer Valley Graben: an overview, Geologie en Mijnbouw 73: 95–98.Google Scholar
Van den Berg, M.W., 1996. Fluvial sequences of the Maas - a 10 Ma record of neotectonics and climate change at various time-scales. Ph.D-thesis, Agricultural University, Wageningen: 181 pp.Google Scholar
Zagwijn, W.H., 1989. The Netherlands during the Tertiary and Quaternary: a case history of coastal lowland evolution. Geologie en Mijnbouw 68: 107–120.Google Scholar
Zagwijn, W.H., 1996. The Cromerien Complex Stage of the Netherlands and correlation with other areas in Europe. In: Turner, C. (ed.): The early Middle Pleistocene in Europe. Proc. SEQS Cromer symposium, Balkema (Rotterdam): 145–172.Google Scholar