Hostname: page-component-cc8bf7c57-l9twb Total loading time: 0 Render date: 2024-12-10T08:29:13.676Z Has data issue: false hasContentIssue false

The coversands and timing of Late Quaternary earthquake events along the Peel Boundary Fault in the Netherlands

Published online by Cambridge University Press:  01 April 2016

M. Frechen*
Affiliation:
Universität Regensburg, Institut für Geographie, D-93040 Regensburg, Germany
M.W. van den Berg
Affiliation:
Netherlands Institute of Applied Geoscience TNO, National Geological Survey, Dr. van Deenweg 130, P.O. Box 511, NL-8000 AM Zwolle, The Netherlands Email:m.vandenberg@nitg.tno.nl
*
Corresponding address: Institut für Geowissenschaftliche Gemeinschaftsaufgaben (GGA), S 3: Geochronology and Isotope Hydrology, Stilleweg 2, D-30655 Hannover, Germany Email: M.Frechen@gga-hannover.de
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

The coversands along the Peel Boundary Fault in the Netherlands were investigated by a luminescence dating approach combining Infrared Optically Stimulated Luminescence (IRSL) and Thermoluminescence (TL) methods. At the Neer trench, ten samples were collected and investigated in order to set up an independent chronological framework for the deposition history of the fluvio-aeolian and aeolian sediments and hence the timing of Late Weichselian and Holocene earthquake events. Five sedimentary units could be distinguished by this chronological approach. The oldest fluvio-aeolian unit yielded a mean deposition age of 35.9±0.4 ka and is designated to correlate with the Middle Weichselian. An IRSL age estimate of 20.1 ±2.9 ka was determined for the sediment that most likely represents the Older Coversands I, and a mean luminescence age of 15.1±1.2 ka for deposits just below the Beuningen gravel bed. The aeolian sediment from above the Beuningen horizon yielded an IRSL age estimate of 9.4±1.0 ka. The youngest deposits from the colluvial wedge yielded <6.9±0.7 ka BP, and so an earthquake event was likely to occur during the Middle or Late Holocene, as evidenced by the luminescence age estimates.

Type
Special section: Palaeosis ECGS/CEGS additional papers
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2002

References

Ahorner, L., 1994. Fault-plane solutions and source parameters of the 1992 Roermond, The Netherlands, mainshock and its stronger aftershocks from regional seismic data. Geologie en Mijnbouw 73: 199–214.Google Scholar
Bateman, M.D. & van Huissteden, K., 1999. The timing of lastglacial periglacial and aeolian events, Twente, eastern Netherlands. Journal of Quaternary Science 14: 277–283.3.0.CO;2-W>CrossRefGoogle 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.CrossRefGoogle Scholar
Dijkmans, J.W.A., van Mourik, J.M. & Winde, A.G., 1992. Thermoluminescence dating of aeolian sands from polycyclic soil profiles in southern Netherlands. Quaternary Science Reviews 11: 85–92.CrossRefGoogle Scholar
Dijkmans, J.W.A., Wintle, A.G. & Mejdahl, V., 1988. Some thermoluminescence properties and dating of eolian sands from the Netherlands. Quaternary Science Reviews 7: 349–355.CrossRefGoogle Scholar
Frechen, M., Vanneste, K., Verbeek, K., Paulissen, E. & Camelbeeck, T., 2001. The deposition histoty of the coversands along the Bree Fault Escarpment, NE Belgium. Netherlands Journal of Geosciences/Geologie en Mijnbouw 80: 171–185.Google Scholar
Frechen, M., Dermann, B., Boenigk, W. & Ronen, A., 2001b. Luminescence chronology of aeolianites from the section at Givat Olga — Coastal Plain of Israel. Quaternary Science Reviews 20: 805–809.CrossRefGoogle Scholar
Frechen, M., van Vliet-Lanoë, B. & Vandenhaute, P., 2001c. The Upper Pleistocene loess record at Harmignies/Belgium - high resolution terrestrial archive of climate forcing. Palaeogeography Palaeoclimatology Palaeoecology, 173: 175–195.CrossRefGoogle Scholar
Geluk, M.C., Duin, E.J.T., Dusar, M., 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
Hoek, W., 1997. Paleogeography orlate glacial vegetation. PhD thesis, Free University Amsterdam, 147 pp.Google Scholar
Huntley, D.J. & Barril, M.R., 1997. The K content of the K-feldspars being measured in optical dating or in thermoluminescence dating. Ancient TL 15: 11–13.Google Scholar
Poolton, N.R.J., et al., 1996. Luminescence dating of sediments from Panheel. Boreas 25: 195–208.Google Scholar
Prescott, J.R. & Robertson, G.B., 1997. Sediment dating by luminescence: a review. Radiation Measurements 27: 893–922.CrossRefGoogle Scholar
Stuiver, M., Grootes, P.M. & Braziumas, T.F., 1995. The GISP-2 δ18O climate record of the past 16,500 years and the role of the sun, ocean, and volcanoes. Quaternary Research 44: 314–354.CrossRefGoogle Scholar
Van den Berg, M.W. & Frechen, M., in preparation. Luminescence chronology of the Panheel type site. To be submitted to Geologie en Mijnbouw.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. Thesis University of Wageningen, pp. 182.Google Scholar
Van den Berg, M.W. & Lokhorst, A., 2000. Paleoseismic investigations along the Peel boundary fault: geological setting, site selection and trenching results. Conference proceedings HAN2000-potential for large earthquakes in low seismic activity regions of Europe, pp. 139–144; Han-sur-Lesse.Google Scholar
Vanneste, K., Maghraoui, M. & Camelbeeck, T. 1999. Late Quaternary earthquake-related soft-sediment deformation along the Belgian portion of the Feldbiss Fault, Lower Rhine Graben system. Tectonophysics 309: 57–79.CrossRefGoogle Scholar
Vanneste, K., Verbeeck, K., Camelbeeck, T., Renardy, F., Jongmans, S.D., Meghraoui, M., Paulissen, E., Frechen, M., 2001. Surface rupturing history of the Bree fault escarpment, Roer Valley Graben: new trench evidence for at least six successive events during the last 150 to 185 kyr. Journal of Seismology. 5: 329–359.CrossRefGoogle Scholar
Wallinga, J. & Duller, G.A.T., 2000. The effect of optical absorption on the infrared stimulated luminescence age obtained on coarse-grain feldspar. Quaternary Science Reviews 19: 1035–1042.CrossRefGoogle Scholar
Winde, A.G., 1997. Luminescence dating: laboratory procedures and protocols. Radiation Measurements 27: 769–817.Google Scholar