Variations in slow slip moment rate associated with rapid tremor reversals inC ascadia
| Autor: | Alexandra A. Royer, Michael G. Bostock, J. C. Hawthorne, Amanda M. Thomas |
|---|---|
| Rok vydání: | 2016 |
| Předmět: |
musculoskeletal diseases
Strain energy release rate 010504 meteorology & atmospheric sciences Slip (materials science) Strainmeter Strain rate 010502 geochemistry & geophysics 01 natural sciences body regions Stress drop Plate tectonics Geophysics Geochemistry and Petrology Forward propagation Aseismic slip Geology Seismology 0105 earth and related environmental sciences |
| Zdroj: | Geochemistry, Geophysics, Geosystems. 17:4899-4919 |
| ISSN: | 1525-2027 |
| Popis: | During large slow slip events, tremor sometimes propagates in the reverse along-strike direction for a few hours, at speeds 10 to 40 times faster than the forward propagation. We examine the aseismic slip that underlies this rapidly propagating tremor. We use PBO (Plate Boundary Observatory) borehole strainmeter data to search for variations in the slow slip moment rate during 35 rapid tremor reversals (RTRs) that occurred beneath Vancouver Island. The strain records reveal that, on average, the strain rate increases by about 100% ( ±30%) during RTRs. Given the Green's functions expected for slip in the RTR locations, these strain rate increases imply 50 to 130% increases in the aseismic moment rate. The median moment released per RTR is between 8 and 21% of the daily slow slip moment, equivalent to that of a MW 5.0 to 5.1 earthquake. By combining the RTR moments with the spatial extents suggested by tremor, we estimate that a typical RTR has peak slip of roughly one-sixth of the peak slip in the main slow slip event, near-front slip rate of a few to ten times the main front slip rate, stress drop around half the main event stress drop, and strain energy release rate around one-tenth that of the main front. Our observations support a picture of RTRs as aseismic subevents with high slip rates but modest strain energy release. RTRs appear to contribute to but not dominate the overall slow slip moment, though they may accommodate most of the slip in certain locations. |
| Databáze: | OpenAIRE |
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