Titlebook: Seismic Activity in Western Europe; with Particular Cons Paul J. Melchior Book 1985 D. Reidel Publishing Company, Dordrecht, Holland 1985 a

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The General Pattern of Seismotectonic Dislocations in Central Europe as the Background for the Liègee-spread regional stress field within the Earth’s crust characterized by a rather uniform trend of the maximum compressive stress in NW-SE direction (145° with respect to North). The second controlling factor is the post-Hercynian block mosaic and the existence of deep reaching major fault structure

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Seismicity of Western Europe as Determined from ISC Data Fileslatively low seismic activity to the effects of close shallow earthquakes. An essential first step in understanding the seismicity of an area is the compilation of comprehensive catalogues of earthquakes, and this paper presents plots of events in northwest Europe taken from the files of the Interna

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Some Notes Concerning the Seismicity in Belgium — Magnitude Scale — Detection Capability of the Belguakes in Belgium. The method gives coherent evaluation when applied to earlier data as shown by the study of the Havré earthquake of April 3, 1949.In addition, the cumulative frequency distribution of earthquakes felt in Belgium and the detection capability of the belgian seismological stations are

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