Abstract
The source mechanism of two moderate-size normal-faulting earthquakes located slightly south of the Grand Canyon in Arizona are studied, using several near real-time seismic-wave analysis procedures. The events are found to have source depths near 10 to 15km, and the smaller of the two events (mb=4.8) is used to provide Empirical Green's Functions to analyze the rupture directivity of the larger (Mw=5.3) mainshock. These events indicate complexity in the crustal stress environment on the western margin of the Colorado Plateau. -Authors
Original language | English (US) |
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Pages (from-to) | 451-457 |
Number of pages | 7 |
Journal | Bulletin - Seismological Society of America |
Volume | 84 |
Issue number | 2 |
State | Published - 1994 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Geochemistry and Petrology