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Titlebook: Earthquake Hazard and Risk; Vladimír Schenk Book 1996 Kluwer Academic Publishers 1996 Geoinformationssysteme.aftershock.earthquake.microse

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发表于 2025-3-21 17:13:14 | 显示全部楼层 |阅读模式
书目名称Earthquake Hazard and Risk
编辑Vladimír Schenk
视频video
丛书名称Advances in Natural and Technological Hazards Research
图书封面Titlebook: Earthquake Hazard and Risk;  Vladimír Schenk Book 1996 Kluwer Academic Publishers 1996 Geoinformationssysteme.aftershock.earthquake.microse
描述.Earthquake Hazard and Risk. is a book summarizing selectedpapers presented at the 27th General Assembly of the InternationalAssociation of Seismology and Physics of the Earth‘s Interior(Wellington, January 1994). .The papers, rigorously scrutinized by an international board ofreferees, cover some recent aspects of current research in earthquakehazard and seismic risk. They address the algorithms and methodologyused in seismological applications, the reliability of thesetechniques with the decreasing level of probability and uncertaintyassociated with various seismotectonic settings, the physical andstatistical nature of earthquake occurrences, strong ground motionsand effects of surface seismogeological conditions. A special efforthas been made to include papers that illustrate the assessment ofearthquake hazard and seismic risk through applications at sites ineither inter-plate or intra-plate tectonic settings. Of particularinterest is hazard assessment in regions of rare large earthquakes..The book is suitable for those interested in earthquake hazard andseismic risk research as well as a more general audience ofseismologists, geophysicists and Earth scientists. It is also usefu
出版日期Book 1996
关键词Geoinformationssysteme; aftershock; earthquake; microseism; seismic; seismology; hydrogeology
版次1
doihttps://doi.org/10.1007/978-94-009-0243-5
isbn_softcover978-94-010-6592-4
isbn_ebook978-94-009-0243-5Series ISSN 1878-9897 Series E-ISSN 2213-6959
issn_series 1878-9897
copyrightKluwer Academic Publishers 1996
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The Probability of the Time Occurrence of Strong Earthquake for Some Zones in Albaniaones and lines of Albania, in this paper we have made use of property that the time interval sequence of earthquakes follows the logarithmic normal distribution, as proved by the test of normality..Eventually, for the different seismic regions we obtained the different time interval that the next st
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Statistical Estimation of the Maximum Magnitude and its Uncertainty from a Catalogue Including Magniually there are errors in earthquake magnitudes of modern and historic events. Taking into account the standard deviations of errors in earthquake magnitudes results in modified distribution of observed magnitudes. The new magnitude distribution slightly differs from the Gutenberg-Richter’s one for
发表于 2025-3-22 05:23:36 | 显示全部楼层
Estimation of Upper Bound Magnitude in Earthquake Hazard Assessment in Sloveniaified causative faults. The analysis of the earthquake catalogue of Slovenia and surrounding areas showed that for the region of Slovenia a doubly truncated exponential frequency-magnitude relationship may serve directly for this purpose, taking into account the following assumptions:.(1) The value
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Changes of the State of Stress and Deformation in Epicentral Zones During the Aftershock Periodes and a prediction of strong aftershocks. The high precision geodetic, magnetometric and gravimetric repeated measurements after a main shock have been carried out in the epicentral zones of earthquakes with M≥7..During a gradual descent of seismic activity, the trend and oscillatoring changes of g
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Preliminary Seismic Hazard Assessment for the Italian Seismic Coderesented. They have been obtained by applying two methodologies (the Cornell approach and the mixed method), and refer to two stages of elaboration: after having summarised the products performed during a previous national project, and after the first release of the products developed ad hoc for the
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Earthquake Hazard Assessment for the Czech Republic and Adjacent Areaoth a review of the calculations obtained and an outlook of possible new methodological aspects in earthquake hazard calculations are summarized. The hazard calculations have been made mainly for the region of 48.5°-51.2°N, 12°-19°E, which belongs to an area of relatively low seismicity, and which i
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