Resumo

VIDAL, Antonio  e  MUNGUIA, Luis. A new coda-duration magnitude scale for northern Baja California, Mexico. Geofís. Intl [online]. 2005, vol.44, n.1, pp.11-22. ISSN 2954-436X.

ABSTRACT

In northern Baja California, coda-durations of seismic signals recorded in the sediments of the Mexicali-Imperial Valley (MIV) are longer than those recorded on the granitic Peninsular Ranges of Baja California (PRBC). The source-receiver distance and the local geology conditions also affect coda duration. Using data from earthquakes in the 1.8-to-5.8-magnitude range, we performed a multiple regression analysis to get two new duration magnitude relationships as follows: MD = - (1.56 ± 0.21) + (2.44 ± 0.13) log ʈ + (0.0023 ± 0.0004) ʈ + S, for PRBC, and MD = - (1.27 ± 0.38) + (2.31 ± 0.20) log ʈ + (0.0012 ± 0.0004) ʈ + S, for MIV, where ʈ and S are lapse-time values and station corrections, respectively. Station corrections range from -0.60 to +0.19. The new magnitudes are calibrated with a local magnitude scale previously defined for the region.

Palavras-chave : Duration magnitude; coda-duration; station correction.

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