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Titlebook: Digital Seismology and Fine Modeling of the Lithosphere; R. Cassinis,G. Nolet,G. F. Panza Book 1989 Springer Science+Business Media New Yo

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發(fā)表于 2025-3-21 19:53:46 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Digital Seismology and Fine Modeling of the Lithosphere
編輯R. Cassinis,G. Nolet,G. F. Panza
視頻videohttp://file.papertrans.cn/280/279656/279656.mp4
叢書名稱Ettore Majorana International Science Series
圖書封面Titlebook: Digital Seismology and Fine Modeling of the Lithosphere;  R. Cassinis,G. Nolet,G. F. Panza Book 1989 Springer Science+Business Media New Yo
出版日期Book 1989
關鍵詞lithosphere; modeling; seismology
版次1
doihttps://doi.org/10.1007/978-1-4899-6759-6
isbn_softcover978-1-4899-6761-9
isbn_ebook978-1-4899-6759-6
copyrightSpringer Science+Business Media New York 1989
The information of publication is updating

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https://doi.org/10.1007/978-3-642-14840-8ervations of travel time anomalies. The deployment of broad-band instrumentation and advances in analysis methods now permit more extensive use of waveform data to model slab effects, including those that are non-geometrical.
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Very-Broad-Band Seismometry,ists in Japan in 1880. Most of their instruments were designed to record the largest possible range of periods. The Japanese seismologist Omori recorded beautiful broad-band seismograms of large earthquakes around 1900 which until recently one could not have obtained with modern seismographs.
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Wave Propagation in Subducted Lithospheric Slabs,ervations of travel time anomalies. The deployment of broad-band instrumentation and advances in analysis methods now permit more extensive use of waveform data to model slab effects, including those that are non-geometrical.
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Francesco Massari,Hildegard Westphalthat processing. Although every seismic line has its own individual processing problems, the standard processes appropriate to almost all marine deep reflection data are shown here, so that this paper may serve both as a tutorial to workers entering this field and as a reivew of a standarized processing sequence presently in use at BIRPS.
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