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 …
Recurring slow slip along near-trench megathrust faults occurs at many subduction zones, but for unknown reasons, this process is not universal. Fluid overpressures are implicated in …
H Okuda, AR Niemeijer, M Takahashi… - Journal of …, 2023 - Wiley Online Library
Nucleation of earthquake slip at the plate boundary fault (décollement) in subduction zones has been widely linked to the frictional properties of subducting sedimentary facies …
Rapid tremor migration (RTM) in subduction zones is a manifestation of complex fault-zone processes on the plate interface. Recent observations have revealed a large diversity of …
Abstract The Ras El Ush field (Gulf of Suez, Egypt) is characterized by various complex structural features, such as evaporite deposits and faulting. Such complex geologic setting …
The fluid‐flow properties of fractures have received increasing attention regarding the role of geofluids in the genesis of slow and fast earthquakes and recent advances in …
The spatial distributions of shallow slow earthquakes are related to stress accumulation and structural characteristics of the shallow plate boundary, which are important for …
H Okuda, M Kitamura, M Takahashi… - Earth and Planetary …, 2023 - Elsevier
Along subduction zone megathrust faults, the transition from smectite to illite with depth occurs at temperatures of∼ 150° C and has long been hypothesized to be one of the …
R Kamei, D Lumley - Geophysical Journal International, 2017 - academic.oup.com
Seismic monitoring provides valuable information regarding the time-varying changes in subsurface physical properties caused by natural or man-made processes. However, the …