[S-CG44] Science of slow-to-fast earthquakes

[SCG44-17] A search for long-term slow slip in Cascadia

★Invited Papers

*Carolyn Nuyen¹、David Schmidt¹ (1.University of Washington Seattle)

Long-term slow slip events have been observed at several subduction zones around the globe, and they play an integral part in strain release along megathrust faults. Nevertheless, evidence for long-term slow slip has remained elusive in the Cascadia subduction zone. Here we conduct a systematic analysis of thirteen years of GNSS time series data from 2006-2019 and present evidence of at least one low-amplitude long-term slow slip event on the Cascadia subduction zone, with the possibility of others that are less resolved. Starting in mid 2012, a 1.5-year transient is observed in southern Cascadia, with a group of coastal GNSS stations moving ~2 mm to the west. The data are modeled as a Mw 6.4 slow slip event occurring at 15-35 km depth on the plate interface, just up-dip of previously recognized short-term slow slip and tremor. The event shares many characteristics with similar long-term transient events on the Nankai subduction zone. However, the total fault slip amplitude is an order-of-magnitude smaller in Cascadia when compared to large events elsewhere, making long-term slow slip detection challenging in Cascadia.