Abstract
From 1940 to 1983 no earthquakes in the southern part of The Netherlands with a magnitude smaller than two are detected. This study shows that detection and location of earthquakes with magnitude two or lower with the existing network is mostly impossible and that the capability to detect and locate can be improved only by an extention of the seismic network
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References
Ritsema, A.R., 1966, Note on the seismicity of the Netherlands, Proceedings Kon. Ned. Akademie van Wetenschappen, Series B, 69, no. 2, pp. 235–239
Ahorner, L., a. o., 1976, First draft of an earthquake zoning map of Northwest Germany, Belgium, Luxemburg and the Netherlands, Proceedings of the E.S.C. Symposium in Luxemburg on Earthquake risk for nuclear power plants, pp. 39–41, KNMI, De Bilt
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Ritsema, A.R., 1983, Note on the detection and location capability of the Netherlands seismic stations for earthquakes in the North Sea Basin, Proceedings of the NATO advanced study workshop on Seismicity and Seismic Risk in the Offshore North Sea Area, pp. 195–197, D. Reidel Publishing Company, Dordrecht
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© 1985 D. Reidel Publishing Company
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de Crook, T. (1985). The Problem of Micro-Earthquakes in the Southern Part of the Netherlands. In: Melchior, P.J. (eds) Seismic Activity in Western Europe. NATO ASI Series, vol 144. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-5273-7_11
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DOI: https://doi.org/10.1007/978-94-009-5273-7_11
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-8829-9
Online ISBN: 978-94-009-5273-7
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