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Titlebook: Identification of Seismic Sources — Earthquake or Underground Explosion; Proceedings of the N Eystein S. Husebye,Svein Mykkeltveit Conferen

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书目名称Identification of Seismic Sources — Earthquake or Underground Explosion
副标题Proceedings of the N
编辑Eystein S. Husebye,Svein Mykkeltveit
视频video
丛书名称Nato Science Series C:
图书封面Titlebook: Identification of Seismic Sources — Earthquake or Underground Explosion; Proceedings of the N Eystein S. Husebye,Svein Mykkeltveit Conferen
描述The subject of this NATO Advanced Study Institute was seismic monitoring under a nuclear test ban - an application of scienti­ fic knowledge and modern technology for a political purpose. The international political objective of a comprehensive nuclear test ban provided in turn the motivation for our technical and scientific discussions. In order to obtain a historical perspec­ tive on the progress of the work towards a comprehensive test-ban treaty (CTB), it is necessary to go back to 1958, when a confer­ ence of scientific experts in Geneva made the first steps toward an international seismic monitoring system. However, agreement on actual capabilities of a monitoring system for verifying compliance with such a treaty was not achieved, and thus the conference did not lead to immediate political results. After the Partial Test Ban Treaty of 1963, which banned nuclear explosions in the atmosphere, outer space and under the seas, renewed interest in the seismological verification of a CTB took place. A number of countries initiated large-scale research efforts toward detecting and identifying underground nuclear explosions, and it was in this context that the large­ aperture seismic
出版日期Conference proceedings 1981
关键词atmosphere; earthquake; scattering; seismic; seismometer
版次1
doihttps://doi.org/10.1007/978-94-009-8531-5
isbn_softcover978-94-009-8533-9
isbn_ebook978-94-009-8531-5Series ISSN 1389-2185
issn_series 1389-2185
copyrightD. Reidel Publishing Company, Dordrecht, Holland 1981
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Dynamics of Seismic Sourcesen a circular crack model and its radiation; this is the model most seismologists use to invert source parameters. Finally, we review some recent propositions to explain earthquake complexity and multiple events. Seismic moments, stress drops and corner frequencies may be strongly affected by source complexity.
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The Effect of Green’s Functions on the Determination of Source Mechanisms by the Linear Inversion ofment tensor with the deviatoric component as much as a factor of twenty-five smaller. The time function of the source appears to have a double peaked nature. The fit of the calculated seismograms to the observed is not greatly affected by the assumed Green’s function.
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Some Recent Extensions of the Reflectivity Methodf the reflectivities of different parts of the layered medium. Each case is illustrated with an example of theoretical seismograms. Finally, a few remarks are made on aliasing in the time domain, on fast Hankel transforms and on causal absorption with frequency-dependent Q-factor.
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Seismic Moment Tensorstions which are hoped to bridge a gap between abstract formalism and practical requirements. Emphasis is on those practical aspects of moment tensors which are likely to be useful in future applications, and on those theoretical aspects which have led to some confusion in the past.
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