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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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A Just Society for Ireland? 1964-1987stribution, as proved by the test of normality..Eventually, for the different seismic regions we obtained the different time interval that the next strong earthquake might occur..The results may help the study of seismic zoning, microzoning, seismic risk and other problems.
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https://doi.org/10.1007/978-3-319-98092-8et, where a focal mechanism tensor is treated as a random object. The procedure of numerical simulation of random focal mechanism tensors is proposed. We also describe the process of numerical simulation of a set of random focal mechanism tensors corresponding to the given probability density function.
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Critique: Between Theory and Method,fter having summarised the products performed during a previous national project, and after the first release of the products developed ad hoc for the present GNDT project. Maps of horizontal and vertical PGA referring to 100 and 500 year return periods and maps of exceedance probability for intensity VII MCS in 50 years are shown and commented.
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https://doi.org/10.1007/978-3-031-50539-3first the significance and methodology for developing for the Expert System for Earthquake Hazard Assessment abbreviated ESEHA is described; secondly, its content composition, logical structure, knowledge-base, major algorithms, case study and its results are introduced; finally some conclusion and discussion are given.
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Reading the Ancient World with Chicano Eyes,arried out in the framework of GNDT (National protection Against Earthquake of the National Council of Research).data base of observed intensities compiled by the same research group..Significant differences were found which, in particular, show the importance of observed site intensities for a reliable hazard assessment.
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