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Evidence for tidal triggering of high-amplitude rapid tremor reversals and tremor streaks in northern Cascadia
We provide a new link between tectonic tremor propagation, tremor amplitude, and tidal stresses by analyzing high‐resolution tremor locations and amplitudes determined by multibeam backprojection of data from an array of subarrays. For two Cascadia episodic tremor and slip events, we observe repeati...
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Published in: | Geophysical research letters 2013-08, Vol.40 (16), p.4254-4259 |
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Main Authors: | , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | We provide a new link between tectonic tremor propagation, tremor amplitude, and tidal stresses by analyzing high‐resolution tremor locations and amplitudes determined by multibeam backprojection of data from an array of subarrays. For two Cascadia episodic tremor and slip events, we observe repeating, high‐amplitude rapid tremor reversals (RTRs) and tremor streaks. They tend to occur when tremor amplitudes are highest and occur almost exclusively during periods of thrust‐encouraging, tidally induced shear stress on the fault. We speculate that thrust‐encouraging shear stress from tidal loading forces trigger RTRs and streaks that energetically rerupture the weakened fault behind the slow slip front. The high rate and amplitude of tremor during RTRs and streaks stands in contrast to the hypothesis that activity at the leading edge of the slow slip zone is the most energetic and loudest. This implies that the spatiotemportal pattern of slow earthquake slip migration is even more intricate than previously reported.
Key Points
RTR's and streaks are high in amplitude relative to tremor at the slip front
RTR's and streaks occur during slip‐encouraging tidal shear stress
RTR's and streaks may be triggered by tidal loading and tidal stresses |
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ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1002/grl.50832 |