Results from Rupture Directivity of Moderate Earthquakes in Northern California
by Linda Seekins and John Boatwright
We analyzed the directivity for 47 moderate 3.5≤M≤5.4 earthquakes that occurred between 1998 and 2008. View the solutions for these earthquakes.
The map shows the locations of 36 of the earthquakes analyzed: one event near Mammoth Lakes, three events in Humboldt county, and four events near Paso Robles are located outside of the map. The small dots represent Shakemap recording stations.
Distribution of Rupture Direction and Velocity
The earthquakes we have analyzed for directivity comprise 35 strike-slip earthquakes, 11 thrust earthquakes, and 1 normal-faulting earthquake.
Rupture directions for the 33 strike-slip earthquakes analyzed, these directions are plotted as they would be seen from the southwest for northwest striking faults and from the southeast for northeast striking faults.
Rupture directions for the 9 thrust and 2 normal faulting earthquakes analyzed: these directions are plotted as they would be viewed looking down on the faults.
Rupture velocity distribution for the PGA inversions. To obtain these rupture velocities, we relaxed the limit of ν ≤ 0.92β : four inversions obtained transonic rupture velocities β < ν ≤ α. The blue area represents a smoothed average.
Rupture velocity distribution for the PGV inversions. Three inversions obtained transonic rupture velocities β < ν ≤ α. The yellow area represents a smoothed average.
The most striking result of the study is the prevalence of strong directivity in the peak ground motions. The second striking result of this study is the tendency for strike-slip earthquakes to rupture updip.