G&T Seminar on Deep Earthquakes

This summer I gave an online seminar as part of the Geophysics & Tectonics Seminar hosted by Keely O’Farrell at the University of Kentucky (seminar recording on youtube).  In this seminar I present the hypothesis that strain-rate is an important factor in determining where earthquakes occur in subducting slabs, because strain-rate is a factor that affects the proposed triggering mechanisms for  deep earthquakes.