Seismic waves in complex 3-D structures. Report 23

0423498 - GFÚ 2014 CZ eng M - Část monografie knihy
Jechumtálová, Zuzana - Bulant, P.
Effects of 1-D versus 3-D velocity models on moment tensor inversion in the Dobrá Voda locality at the Little Carpathians region, Slovakia.
Seismic waves in complex 3-D structures. Report 23. Prague: Charles University, 2013, s. 253-269
Grant CEP: GA ČR GAP210/10/1728
Institucionální podpora: RVO:67985530
Klíčová slova: ray tracing * 3-D velocity model * earthquake mechanism * amplitude inversion
Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země

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.
Trvalý link: http://hdl.handle.net/11104/0229678