Spatiotemporal slip distributions associated with the 2018-2019 Bungo Channel long-term slow slip event inverted from GNSS data.

ABSTRACT: Long-term slow slip events (L-SSEs) have repeatedly occurred beneath the Bungo Channel in southwestern Japan with durations of several months to a couple of years, with a recurrence interval of approximately 6 years. We estimated the spatiotemporal slip distributions of the 2018-2019 Bungo Channel L-SSE by inverting processed GNSS time series data. This event was divided into two subevents, with the first on the southwest side of the Bungo Channel from 2018.3 to 2018.7 and the second beneath the Bungo Channel from 2018.8 to 2019.4. Tectonic tremors became active on the downdip side of the L-SSE occurrence region when large slow slips took place beneath the Bungo Channel. Compared with the previous Bungo Channel L-SSEs, this spatiotemporal slip pattern and amount were similar to those of th

SUBMITTER: Seshimo Y 

PROVIDER: S-EPMC8748931 | biostudies-literature | 2022 Jan

REPOSITORIES: biostudies-literature