EES Guest Speaker - Dr. Peter Shearer
This week’s seminar speaker is Dr. Peter Shearer! Please join us Thursday September 5th, 2024 at 3pm in room 351 Nat Sci.
Title:
Adventures in Measuring Variations in High-Frequency Radiation for Small to Moderate
                     Earthquakes
Abstract:
Earthquake stress drop is a key parameter for understanding fault ruptures and estimating
                     strong ground motions, but stress-drop estimates vary widely among different groups.
                     Traditional methods for measuring earthquake stress drop for small earthquakes (M
                     < 5) rely on analysis of P- and S-wave spectra. Similar-sized earthquakes vary in
                     the strength of their high-frequency radiation and various modeling assumptions can
                     be used to translate these differences into stress-drop estimates. Based on our recent
                     work documenting hard-to-resolve tradeoffs between absolute stress drop, stress-drop
                     scaling with moment, high-frequency fall-off rate, and empirical corrections for path
                     and attenuation terms, we adopt a new approach in which the corner frequencies of
                     the smallest earthquakes in each region are fixed to a constant value. This removes
                     any true coherent spatial variations in stress drops among the smallest events but
                     ensures that any spatial variations seen in larger-event stress drops are real and
                     not an artifact of inaccurate path corrections. Applying this approach across southern
                     California, we document spatial variations in stress drop for M 1.5 to 4 earthquakes
                     that agree with previous work, such as lower-than-average stress drops in the Salton
                     Trough, as well as small-scale stress-drop variations along many faults and aftershock
                     sequences. However, our results are unable to independently determine the average
                     stress drop for small earthquakes, highlighting the limitations of purely empirical
                     approaches to spectral analysis for earthquake source properties and the importance
                     of determining shallow crustal attenuation models.


