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Imaging evolution of Cascadia slow-slip event using high-rate GPS
Yuji Itoh1,2, Yosuke Aoki3, Junichi Fukuda3
1Earthquake Research Institute, The University of Tokyo, Bunkyo-ku, Tokyo, 113-0032, Japan. yuji.itoh@univ-grenoble-alpes.fr.
Scientific Reports
|May 3, 2022
Summary
High-resolution Global Positioning System (GPS) data reveals sub-daily processes during slow slip events (SSEs). This advanced analysis provides unprecedented detail on SSE evolution and mechanisms.
Area of Science:
- Geophysics
- Tectonics
- Seismology
Background:
- Slow slip events (SSEs) are typically studied using daily Global Positioning System (GPS) data.
- Daily data limits the understanding of sub-daily processes and underlying mechanisms of SSEs.
Purpose of the Study:
- To investigate the potential of sub-daily kinematic GPS analysis for imaging SSEs.
- To overcome the temporal resolution limitations of traditional daily GPS data.
Main Methods:
- Applied post-processing techniques to 30-minute kinematic GPS data to reduce non-tectonic noise.
- Inverted high-temporal-resolution GPS data to create spatiotemporal slip images of an SSE.
- Compared results with inversions from daily GPS data.
Main Results:
- Successfully captured transient motions of a few millimeters during a Cascadia SSE using 30-minute GPS data.
- Revealed a multi-stage SSE evolution: isotropic growth followed by along-strike migration.
- Observed slip behavior similar to regular earthquake ruptures, suggesting common mechanical factors.
Conclusions:
- Sub-daily kinematic GPS analysis is feasible for SSE studies, offering improved temporal resolution.
- The findings suggest shared mechanical principles between SSEs and regular earthquakes.
- Further refinement of noise reduction in kinematic GPS analysis will enhance SSE detection and imaging.
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