THE ZIHUATANEJO, MEXICO, EARTHQUAKE OF 1994 DECEMBER 10 (M = 6.6) - SOURCE CHARACTERISTICS AND TECTONIC IMPLICATIONS

An analysis of the Zihuatanejo, Mexico, earthquake of 1994 December 10 (M = 6.6), based on teleseismic and near-source data, shows that it w as a normal-faulting, intermediate-depth (H = 50 +/- 5 km) event. It w as located about 30 km inland, within the subducted Cocos plate. The p referred fault plane has an azimuth of 130 degrees, a dip of 79 degree s and a rake of -86 degrees. The rupture consisted of two subevents wh ich were separated in time by about 2s, with the second subevent occur ring downdip of the first. The measured stress drop was relatively hig h, requiring a Delta sigma of about a kilobar to explain the high-freq uency level of the near-source spectra. A rough estimate of the thickn ess of the seismogenic part of the oceanic lithosphere below Zihuatane jo, based on the depth and the rupture extent of this event, is 40 km. This event and the Oaxaca earthquake of 1931 January 15 (M = 7.8) are the two significant normal-faulting, intermediate-depth shocks whose epicentres are closest to the coast. Both of these earthquakes were pr eceded by several large to great shallow, low-angle thrust earthquakes , occurring updip. The observations in other subduction zones show jus t the opposite: normal-faulting events precede, not succeed, updip, th rust shocks. Indeed, the thrust events, soon after their occurrence, a re expected to cause compression in the slab, thus inhibiting the occu rrence of normal-faulting events. To explain the occurrence of the Zih uatanejo earthquake, we note that the Cocos plate, after an initial sh allow-angle subduction, unbends and becomes subhorizontal. In the regi on of the unbending, the bottom of the slab is in horizontal extension . We speculate that the large updip seismic slip during shallow, low-a ngle thrust events increases the buckling of the slab, resulting in an incremental tensional stress at the bottom of the slab and causing no rmal-faulting earthquakes. This explanation may also hold for the 1931 Oaxaca event.