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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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书目名称Seismic Activity in Western Europe
副标题with Particular Cons
编辑Paul J. Melchior
视频video
丛书名称Nato Science Series C:
图书封面Titlebook: Seismic Activity in Western Europe; with Particular Cons Paul J. Melchior Book 1985 D. Reidel Publishing Company, Dordrecht, Holland 1985 a
描述A damaging earthquake with intensity VII MSK and local magni= tude 5. 1 occurred on November 8, 1983, at 0:49 GMT near the Belgium town of Liege in the border region between Belgium, Germany and the Netherlands. This most severe earthquake in the northwestern part of Central Europe since more than thirty years has well been recorded by the dense seismic station network in West Germany which consists of more than twenty stations situated in the Lower Rhine Embayment and in the adjoining Rhenish Massif. Most of the stations are equipped with modern digital recording systems. Thus high-quality seismograms are available from the region east and southeast of the epicenter covering a distance range between 70 km and 144 km. From these data the source characteristics of the Liege mainshock and of its largest after= shock have been determined in order to get more information on the seismotectonic processes causing the Liege events. 2. Seismic Station Network During the period of 1976 to 1982 the seismic station network in the Lower Rhine Embayment and in the Rhenish Massif was consi= derably enlarged and mostly equipped with digital recording systems (Figure 1). At present there are more t
出版日期Book 1985
关键词aftershock; earthquake; satellite; seismic; seismology
版次1
doihttps://doi.org/10.1007/978-94-009-5273-7
isbn_softcover978-94-010-8829-9
isbn_ebook978-94-009-5273-7Series ISSN 1389-2185
issn_series 1389-2185
copyrightD. Reidel Publishing Company, Dordrecht, Holland 1985
The information of publication is updating

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https://doi.org/10.1007/978-94-009-5273-7aftershock; earthquake; satellite; seismic; seismology
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General Tectonic Frame of Central Europe with Emphasis Given to Neotectonic Movementscontinents and continental fragments were followed by periods of predominant crustal extension and rifting. Since the Silurian three major cycles are generally recognized: The Caledonian, the Hercynian and the Alpine cycle.
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The Problem of Micro-Earthquakes in the Southern Part of the Netherlandson 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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The Seismic Event of November 9, 1983 Earthquake or Sonic Boomd as a Dutch earthquake. It was found that the conditions for sound propagation in the winter season can be very favourable, but no satisfactory explanation could be constructed for the November 9 event. With the aid of a simple microbarograph one can discriminate earthquakes against acoustic events.
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