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Titlebook: Computational Seismology; V. I. Keilis-Borok,Edward A. Flinn (Technical Dire Book 1972 Consultants Bureau, New York 1972 earthquake.geophy

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发表于 2025-3-21 19:40:18 | 显示全部楼层 |阅读模式
书目名称Computational Seismology
编辑V. I. Keilis-Borok,Edward A. Flinn (Technical Dire
视频videohttp://file.papertrans.cn/234/233120/233120.mp4
图书封面Titlebook: Computational Seismology;  V. I. Keilis-Borok,Edward A. Flinn (Technical Dire Book 1972 Consultants Bureau, New York 1972 earthquake.geophy
描述sense do not grow as fast as computational possi­ This book contains selections from Volumes bilities. I-V of the series "Computational Seismology," which Moreover, for some strange reason, comput­ was initiated a few years ago by the Academy of ers usually create a spirit of haste, though they are Sciences of the USSR. Volume V was still in prepa­ intended to provide time for meditation. In com­ ration when the translation was begun, and the trans­ puterizing seismology, therefore, one must first lations of papers from it were made from manu­ generalize the methods and then make them more scripts. Most of the authors are members of the rigorous mathematically. All relevant data must Department of Computational Geophysics of the In­ be processed jointly. Insofar as is possible, a priori stitute of Physics of the Earth, Moscow. hypotheses should be avoided. Particular attention The series is dedicated to theoretical and must be given to exact formulation of the problem, computational aspects of the analysis of seismolog­ to questions of uniqueness and stability, to the con­ ical data. The present state of this field is typical fidence limits of the results, etc. This general ap­ of
出版日期Book 1972
关键词earthquake; geophysics; seismic; seismology; stability
版次1
doihttps://doi.org/10.1007/978-1-4684-8815-9
isbn_softcover978-1-4684-8817-3
isbn_ebook978-1-4684-8815-9
copyrightConsultants Bureau, New York 1972
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mology," which Moreover, for some strange reason, comput­ was initiated a few years ago by the Academy of ers usually create a spirit of haste, though they are Sciences of the USSR. Volume V was still in prepa­ intended to provide time for meditation. In com­ ration when the translation was begun, a
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Automatic Identification of Seismic Wave Arrivalsin this paper. The classical tables [9] list approximately 60 such waves. The number of phases that can be practically distinguished on one recording is, of course, less and only very rarely exceeds 5–10.
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Jana Zscheischler,Sebastian Roggais approximation is that the travel-time curve (travel times τ (i.) and epicentral distances, Δ(i.)) is calculated by numerical integration, while the amplitudes are found by numerical differentiation of the travel-time curve.
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