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Titlebook: Geophysics in Mining and Environmental Protection; Adam F. Idziak,Ryszard Dubiel Book 2011 Springer-Verlag Berlin Heidelberg 2011 Engineer

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書目名稱Geophysics in Mining and Environmental Protection
編輯Adam F. Idziak,Ryszard Dubiel
視頻videohttp://file.papertrans.cn/384/383900/383900.mp4
概述Numerous step-by-step tutorials which help the reader to learn quickly.A special chapter on next generation.Flash prepares the reader for the future.Includes ten tips on how to protect flash sites fro
叢書名稱GeoPlanet: Earth and Planetary Sciences
圖書封面Titlebook: Geophysics in Mining and Environmental Protection;  Adam F. Idziak,Ryszard Dubiel Book 2011 Springer-Verlag Berlin Heidelberg 2011 Engineer
描述This book contains contributions to the 32nd Polish-Czech-Slovak Symposium on Mining and Environmental Geophysics held in May 2009 in Piechowice (Poland). The papers are related to various aspects of geophysical science such as induced seismicity, engineering seismology, environmental geophysics and geophysics in geology
出版日期Book 2011
關(guān)鍵詞Engineering Geophysics; Engineering Seismology; Environmental Geophysics; Induced Seismicity; industrial
版次1
doihttps://doi.org/10.1007/978-3-642-19097-1
isbn_softcover978-3-642-27040-6
isbn_ebook978-3-642-19097-1Series ISSN 2190-5193 Series E-ISSN 2190-5207
issn_series 2190-5193
copyrightSpringer-Verlag Berlin Heidelberg 2011
The information of publication is updating

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Assessment of Fracture Properties from P-Wave Velocity Distribution,s applied for an explanation of fractures influence on the seismic wave propagation. According to this theory, the fracture stiffness can be assessed on the basis of velocity directional dependence. The measurements made proved experimentally the validity of this approach, specifically for the frequency interval from 500?Hz to 700?kHz.
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https://doi.org/10.1007/978-3-663-01478-2ty fifth layer (of about 3,000?Ωm) was measured on profile 2. Determining the thickness of each layer was difficult because of their complicated geological structure, which was a result of fast and intense glacial movements. It was possible to distinguish parts belonging to the moraine or valley.
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An Analysis of Amplification Effects at Selected Polish Seismic Stations,suggesting very weak site effects. The HVSR curves for induced seismicity and for natural earthquakes are similar but not the same. The difference is visible at low frequencies, where the amplification effect estimated on the basis of local seismic records is apparently larger than for the teleseismic events.
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