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The M=6.6 13 May 1995 Kozani - Grevena earthquake struck a region of low historical seismic activity which includes a 10-year-old triangulation network in northern Greece. After the earthquake, monuments from this network were occupied with GPS to measure co-seismic displacements. Inversion of the co-seismic displacement field to yield a source mechanism is achieved by use of a hybrid simplex - Monte-Carlo method which requires no a priori constraints. The model focal mechanism agrees well with the global CMT solution and locally observed aftershocks, but implies a significantly higher scalar moment than do seismological or SAR interferometry studies, and has a longer fault length than the model based on SAR interferometry.
Author(s): Clarke PJ, Paradissis D, Briole P, England PC, Parsons BE, Billiris H, Veis G, Ruegg J-C
Publication type: Article
Publication status: Published
Journal: Geophysical Research Letters
Year: 1997
Volume: 24
Issue: 6
Pages: 707-710
Print publication date: 15/03/1997
ISSN (print): 0094-8276
ISSN (electronic): 1944-8007
Publisher: American Geophysical Union
URL: http://dx.doi.org/10.1029/97GL00430
DOI: 10.1029/97GL00430
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