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 …
Subduction of rough seafloor and seamounts is thought to impact a broad range of geodynamic processes, including megathrust slip behaviour, forearc fluid flow and long-term …
K Obara - Proceedings of the Japan Academy, Series B, 2020 - jstage.jst.go.jp
Slow earthquakes are a recently discovered phenomenon that mainly occur updip and downdip of the seismogenic zones of great earthquakes along the subducting plate …
Various slow earthquakes (SEQs), including tremors, very low frequency events, and slow slip events (SSEs), occur along megathrust zones. In a shallow plate boundary region …
J Pwavodi, ML Doan - Geophysical Journal International, 2024 - academic.oup.com
SUMMARY The Nankai Trough is a locus of slow slip, low-frequency earthquakes, and large magnitude (M w> 8) earthquakes. It is usually assumed that high pore pressure contributes …
Shallow slow earthquakes in subduction zones are related to spatiotemporal variations of stress on the plate boundary adjacent to a megathrust earthquake. A dense network …
S Baba, E Araki, Y Yamamoto, T Hori… - Geophysical …, 2023 - Wiley Online Library
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 …
S Takemura, K Obara, K Shiomi… - Journal of Geophysical …, 2022 - Wiley Online Library
Cross‐correlation analysis was applied to long‐term onshore broadband records from April 2004 to March 2021 to detect and relocate shallow very low frequency earthquakes (VLFEs) …
B Hejrani, H Tkalčić - Journal of Geophysical Research: Solid …, 2020 - Wiley Online Library
Shallow earthquakes in the depth range 0–30 km make up more than 60% of all world's earthquakes. However, resolving their seismic source parameters such as the depth and …