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Publikováno v:
Journal of Geophysical Research: Solid Earth. 86:5053-5060
The recent Oaxaca, Mexico, earthquake November 29, 1978 (MW = 7.6, Ms = 7.8, seismic moment, M0 = 3.2 × 1027 dyne cm), is of special interest because of its location within a predetermined seismic gap. The event excited long-period (100–200 s) mul