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Seismic waves in complex 3-D structures. Report 22
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SYSNO ASEP 0386920 Document Type M - Monograph Chapter R&D Document Type The record was not marked in the RIV Title Effects of 1-D versus 3-D velocity models on moment tensor inversion in the Dobrá Voda locality at the Malé Karpaty region, Slovakia Author(s) Jechumtálová, Zuzana (GFU-E) ORCID, RID
Bulant, P. (CZ)Source Title Seismic waves in complex 3-D structures. Report 22. - Prague : Charles University, 2012 Pages s. 17-27 Number of pages 11 s. Number of pages 184 Publication form Print - P Language eng - English Country CZ - Czech Republic Keywords ray tracing ; 3-D velocity model ; earthquake mechanism ; amplitude inversion Subject RIV DC - Siesmology, Volcanology, Earth Structure R&D Projects GAP210/10/1728 GA ČR - Czech Science Foundation (CSF) Institutional support GFU-E - RVO:67985530 Annotation To retrieve the parameters of a seismic source from seismograms means to deconvolve the response of the medium from the seismic records. Thus, in general, source parameters are determined from both the seismograms and the Green function describing the properties of the medium in which the earthquake focus is buried. The quality of each of these two data sets is equally significant for a successful determination of the source characteristics. As a rule, both the sets are subject to contamination by effects, which decrease the resolution of the source parameters. Seismic records are usually contaminated by noise which appears as a spurious signal not related to the source. Error in the Green function is usually caused by the use of an improper model of the medium due to generally common poor knowledge of the seismic velocity of the area under study. Then, the phenomena of the structure which are not modelled in the Green function are assigned to the source where they distort the source mechanism. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2013
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