A review of shallow slow earthquakes along the Nankai Trough
Slow earthquakes occur at deep and shallow plate boundaries along the Nankai Trough.
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …
Variation in slip behaviour along megathrusts controlled by multiple physical properties
Megathrusts, faults at the plate interface in subduction zones, exhibit substantial
spatiotemporal variability in their slip behaviour. Many previous attempts to discern the …
spatiotemporal variability in their slip behaviour. Many previous attempts to discern the …
Ultralow frictional healing explains recurring slow slip events
Plate motion on shallow subduction megathrusts is accommodated by a spectrum of tectonic
slip modes. However, the frictional properties and conditions that sustain these diverse slip …
slip modes. However, the frictional properties and conditions that sustain these diverse slip …
Observation of shallow slow earthquakes by distributed acoustic sensing using offshore fiber‐optic cable in the Nankai trough, southwest Japan
Abstract Off Cape Muroto area, along the Nankai Trough in southwest Japan, is a typical
area with adjacent occurrences of slow and megathrust earthquakes. High‐resolution …
area with adjacent occurrences of slow and megathrust earthquakes. High‐resolution …
Revisiting seismic energy of shallow tremors: Amplifications due to site and propagation path effects near the Nankai Trough
S Takemura, K Emoto, S Yabe - Journal of Geophysical …, 2024 - Wiley Online Library
We investigated the effects of the propagation path and site amplification of shallow tremors
along the Nankai Trough. Using far‐field S‐wave propagation from intraslab earthquake …
along the Nankai Trough. Using far‐field S‐wave propagation from intraslab earthquake …
Crustal structure of the Nankai subduction zone revealed by two decades of onshore‐offshore and ocean‐bottom seismic data: Implications for the dimensions and …
Two‐decades of onshore‐offshore, ocean‐bottom seismometer, and passive‐source data
are integrated to obtain high‐resolution 3‐D constraints on the architecture of the Nankai …
are integrated to obtain high‐resolution 3‐D constraints on the architecture of the Nankai …
Co‐occurrence of low and very low frequency earthquakes explained from dynamic modeling
Very low‐frequency earthquakes (VLFs) are characterized by longer source duration and
smaller stress drop than regular earthquakes of similar magnitude. Recent studies have …
smaller stress drop than regular earthquakes of similar magnitude. Recent studies have …
Geological fingerprints of deep slow earthquakes: A review of field constraints and directions for future research
Slow earthquakes, including low-frequency earthquakes, tremor, and geodetically detected
slow-slip events, have been widely detected, most commonly at depths of 40–60 km in …
slow-slip events, have been widely detected, most commonly at depths of 40–60 km in …
Detectability analysis of very low frequency earthquakes: methods and application in Nankai using F-net and DONET broad-band seismometers
For a more quantitative discussion of slow earthquake activity, we evaluated the detectable
limits of very low frequency earthquakes (VLFEs), which are seismic slow earthquakes …
limits of very low frequency earthquakes (VLFEs), which are seismic slow earthquakes …
[HTML][HTML] Potential fluid migration process inferred from integrated active-source seismic imaging in the Nankai Trough subduction zone off Cape Muroto, Japan
We investigate the potential fluid migration process in a plate subduction zone on the basis
of integrated active-source seismic imaging from multichannel seismic (MCS) reflection and …
of integrated active-source seismic imaging from multichannel seismic (MCS) reflection and …