| 書目名稱 | Seismic Surface Waves in a Laterally Inhomogeneous Earth |
| 編輯 | V. I. Keilis-Borok |
| 視頻video | http://file.papertrans.cn/864/863906/863906.mp4 |
| 叢書名稱 | Modern Approaches in Geophysics |
| 圖書封面 |  |
| 描述 | Surface waves form the longest and strongest portion of a seismic record excited by explosions and shallow earthquakes. Traversing areas with diverse geologic structures, they ‘a(chǎn)bsorb‘ information on the properties of these areas which is best retlected in dispersion, the dependence of velocity on frequency. The other prop- erties of these waves - polarization, frequency content, attenuation, azimuthal variation of the amplitude and phase - arc also controlled by the medium between the source and the recording station; some of these are affected by the properties of the source itself and by the conditions around it. In recent years surface wave seismology has become an indispensable part of seismological practice. The maximum amplitude in the surface wave train of virtually every earthquake or major explosion is being measured and used by all national and international seismological surveys in the determination of the most important energy parameter of a seismic source, namely, the magnitude M,. The relationship between M, and the body wave magnitude fI1t, is routinely employed in identification of underground nuclear explosions. Surface waves of hundreds of earthquakes recorded ev |
| 出版日期 | Book 1989 |
| 關鍵詞 | earthquake; mining; seismic; economic geology |
| 版次 | 1 |
| doi | https://doi.org/10.1007/978-94-009-0883-3 |
| isbn_softcover | 978-94-010-6885-7 |
| isbn_ebook | 978-94-009-0883-3Series ISSN 0924-6096 |
| issn_series | 0924-6096 |
| copyright | Kluwer Academic Publishers 1989 |
|Archiver|手機版|小黑屋|
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