Energy-to-Moment ratios for Deep Earthquakes: No evidence for scofflaws

Abstract:

Energy-to-moment ratios can provide information on the distribution of seismic source spectrum between high and low frequencies, and thus identify anomalous events (either "slow" or "snappy") whose source violates seismic scaling laws, the former characteristic of the so-called tsunami earthquakes (e.g., Mentawai, 2010), the latter featuring enhanced acceleration and destruction (e.g., Christchurch, 2011). We extend to deep earthquakes the concept of the slowness paramete, Θ=log₁₀E^E/M₀, introduced by Newman and Okal [1998], where the estimated energy E^E is computed for an average focal mechanism and depth (in the range 300-690 km). We find that only minor modifications of the algorithm are necessary to adapt it to deep earthquakes. The analysis of a dataset of 160 deep earthquakes from the past 30 years show that these events scale with an average Θ=-4.34±0.31, corresponding to slightly greater strain release than for their shallow counterparts. However, the most important result to date is that we have not found any "outliers", i.e., violating this trend by one or more logarithmic units, as was the case for the slow events at shallow depths. This indicates that the processes responsible for such variations in energy distribution in the source spectrum of shallow earthquakes, are absent from their deep counterparts, suggesting, perhaps not unexpectedly, that the deep seismogenic zones feature more homogeneous properties than shallow ones. This includes the large event of 30 May 2015 below the Bonin Islands (Θ=-4.13), which took place both deeper than, and oceanwards of, the otherwise documented Wadati-Benioff Zone.