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您的检索式：作者名="Gail M Atkinson"
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| 1 | SOURCE RADIATION AND RESPONSES OF WAVE PROPAGATION显示文摘Recordings of seismic waves propagating from earthquake source to a station at the earth’s surface are a system response function. The convolution operator in time domain can be simplified as a multiplication operator in frequency domain. We discuss in frequency domain the separation of source, path and site effects for global scaling of earthquake source radiation. Also discussed are source scaling model, faulting mechanism, and the H/V inversion problems with crustal and near surface structures. Gross features of apparent source spectra appear to be not much region dependent although there may be difference between tectonic styles within a region of tectonic mixture for which we need further study as data accumulate. Vertical spectra may be a better approach to approximate source radiation, as it has less crustal amplification effects than horizontal spectra. The H/V ratio is evidently a comprehensive indicator of amplification effects from near surface to deep structure. This gives it potential as an inversion tool to deduce site crustal structure. | CHEN Sheng zao 1 and Gail M Atkinson 2 (1. Geomatrix Consultants, Inc., 2101 Webster St., 12 th Floor, Oakland, CA 94612, USA, formerly at Dept. Earth Sciences & Ottawa Carleton Geoscience Center, Carleton University, Ottawa, Canada 2. Dept. Ea | 2001 | Geotectonica et Metallogenia2001，25，1： | 2 |
| 2 | 加拿大西部诱发地震的主因是水压致裂而非废水注入显示文摘在美国中部石油和天然气生产过程中,由于废水的注入而引发了数以百计的小型地震,因此,有人将石油和天然气生产诱发的地震归因于废水注入。但是,在加拿大西部开展的研究结果表明,该地区地震是由生产过程中的水压致裂所致。 | 刘文浩 Gail M Atkinson David W Eaton Hadi Ghofrani | 2016 | 国际地震动态2016，37，5： | 0 |
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