Abstract:A b s t r a c t: Тhe source mechanism of the earthquake occurred on September 1, 1994, with local magnitude M L = 5.2, in the Bitola region in the south-western part of the Republic of Macedonia, was studied in details. The studies included P-nodal planes determination for the earthquake, synthesizing of P-wave traces with the two P-nodal planes taken separately as fault planes, locating of adjacent earthquakes, as well as a comparison of all the obtained results with the results of the previous macroseismic s… Show more
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