Seismic anisotropy observations in the Mexicali Valley, Baja California, México

• Published in: Pure and applied geophysics Vol. 160; no. 12; pp. 2257 - 2278
• Main Authors: GONZALEZ, Mario, MUNGUIA, Luis
• Format: Journal Article
• Language: English
• Published: Basel Springer 01.12.2003; Springer Nature B.V
• Subjects: Anisotropy; Delay; Earth sciences; Earth, ocean, space; Earthquakes; Earthquakes, seismology; Engineering and environment geology. Geothermics; Exact sciences and technology; Geothermics; Internal geophysics; Polarization; Reservoirs; Seismic activity; Seismic phenomena; Seismology; Splitting; Stresses; Trends; Valleys; Mexico; Mexicali Valley; Baja California Mexico; Cerro Prieto; Mexicali Valley; geothermal field; anisotropy; Cerro Prieto; S-waves; accelerograms; preferred orientation; epicenters; earthquakes; North America; microcracks; acceleration; microfractures; depth; geothermal reservoirs; sedimentary cover; fault planes; polarization; stress fields; direction
• ISSN: 0033-4553; 1420-9136
• DOI: 10.1007/s00024-003-2393-1

A study of seismic anisotropy was performed using data from earthquakes of the Mexicali Valley. The investigated region encompasses the Cerro Prieto Geothermal Field (CPGF), one of the most important fields in the world. The results showed that at most of our stations the average polarization directions of the fast S waves range from N14°W to N17°E. A N-S polarization direction was obtained for the whole area by averaging the polarization directions from all stations used. In terms of the EDA hypothesis, this average trend agrees with the postulated state of stress for southern California, and with fault plane solutions for events of the Mexicali Valley. Notorious deviations from the N-S global trend were found southeast of the CPGF, with polarization trends between N25°E and N67°E, and in the geothermal field, with polarization directions between N7°W and N14°W. The polarization results for these zones indicated stress conditions that are different from the more regional stress pattern. The delay times that were measured between the fast and slow shear waves reached values of up to 0.6 sec, with a mean value of 0.35 sec. Consistent with our polarization results, the larger delay times (0.2-0.6 sec) were found in the CPGF. Smaller or null values were observed at the periphery of the study area. No temporal trends in the delay times were apparent, as shown by data from the two stations that recorded the larger number of events. Overall, we conclude that the splitting effects of this study result from a shallow anisotropy volume. The splitting results are thus interpreted as caused by the preferred orientation of vertical fluid-filled microcracks aligned in a direction that is parallel to the regional stress field. The stronger splitting effects that were observed in the area of the CPGF were found consistent with the geothermal reservoir that is embedded in the sedimentary cover of the zone, at depths of 1 to 4-5 km from the surface. We thus believe that such marked splitting effects have a direct relation with the reservoir of the CPGF.[PUBLICATION ABSTRACT]