Detection of small slow slips
Slow slips are a fault slip phenomenon without radiating seismic waves and are attracting attention in relation to earthquakes. Generally, surface displacements due to slow slips are small (several millimeters). Thus, detecting slow slips using GPS data is often difficult. I developed a method for detecting small slow slips and estimating their characteristic parameters, and we applied it to southwest Japan, southcentral Alaska, and northeast Japan. We identified hundreds of slow slips and clarified the physical features of the regions where slow slips occur.
Y. Okada, T. Nishimura, T. Tabei, T. Matsushima, & H. Hirose (2022) Development of a detection method for short-term slow slip events using GNSS data and its application to the Nankai subduction zone. Earth, Planets and Space 74, 18. https://doi.org/10.1186/s40623-022-01576-8
Y. Okada & T. Nishimura (2023) Systematic detection of short-term slow slip events in southcentral Alaska. Geophysical Research Letters 50, e2023GL104901. https://doi.org/10.1029/2023GL104901
Y. Okada & T. Nishimura (2025) Investigation on short-term slow slip events in the northeast Japan subduction zones using decadal GNSS data. Earth, Planets and Space 77, 45. https://doi.org/10.1186/s40623-025-02175-z
T. Nishikawa, T. Nishimura, & Y. Okada (2021) Earthquake swarm detection along the Hikurangi Trench, New Zealand: Insights into the relationship between seismicity and slow slip events. Journal of Geophysical Research: Solid Earth, 126, e2020JB020618. https://doi.org/10.1029/2020JB020618
S. Takemura, Y. Hamada, H. Okuda, Y. Okada, K. Okubo, T. Akuhara, A. Noda, & T. Tonegawa (2023) A review of shallow slow earthquakes along the Nankai Trough. Earth Planets Space 75, 164. https://doi.org/10.1186/s40623-023-01920-6