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 …
Locating boundaries between locked and creeping regions at Nankai and Cascadia subduction zones
EM Sherrill, KM Johnson… - Journal of Geophysical …, 2024 - Wiley Online Library
Interseismic coupling maps and, especially, estimates of the location of the fully coupled
(locked) zone relative to the trench, coastline, and slow slip events are crucial for …
(locked) zone relative to the trench, coastline, and slow slip events are crucial for …
A new mechanical perspective on a shallow megathrust near-trench slip from the high-resolution fault model of the 2011 Tohoku-Oki earthquake
Abstract The 2011 Tohoku-Oki earthquake generated a surprisingly large near-trench slip,
and earth scientists have devoted significant attention to understanding why. Some studies …
and earth scientists have devoted significant attention to understanding why. Some studies …
Geological earthquake simulations generated by kinematic heterogeneous energy-based method: Self-arrested ruptures and asperity criterion
P Venegas-Aravena - Open Geosciences, 2023 - degruyter.com
The lack of clarity regarding slip distribution within heterogeneous rupture areas has a
significant impact on characterizing the seismic source and the role of heterogeneities in …
significant impact on characterizing the seismic source and the role of heterogeneities 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 …
Mechanically Coupled Areas on the Plate Interface in the Kanto Region, Central Japan, Generating Great Earthquakes and Slow‐Slip Events
T Saito, A Noda - Bulletin of the Seismological Society of …, 2023 - pubs.geoscienceworld.org
We detected the mechanically coupled areas, or high stress rate patches, on the plate
interface in the Kanto region, central Japan, by analyzing the Global Navigation Satellite …
interface in the Kanto region, central Japan, by analyzing the Global Navigation Satellite …
MagellanPlus Workshop: mission-specific platform approaches to assessing natural hazards that impact society
Oceanic natural hazards pose threats to coastal communities worldwide. These include
earthquakes, tsunamis, submarine landslide, volcanic eruptions, and tropical cyclones …
earthquakes, tsunamis, submarine landslide, volcanic eruptions, and tropical cyclones …
Differentiating frictionally locked asperities from kinematically coupled zones
DSK Sato, T Hori, Y Fukahata - arXiv preprint arXiv:2409.14266, 2024 - arxiv.org
Seismogenic zones resist slipping before generating earthquakes. Therefore, slip deficit,
also called coupling, is a proxy of interseismic seismogenic zones on plate boundaries …
also called coupling, is a proxy of interseismic seismogenic zones on plate boundaries …
[PDF][PDF] Carvajal-Soto, LA (2024). Deciphering the modern stress field facies in Costa Rica and vicinity from earthquake focal mechanisms and GNSS support)
A López-Saborío - Boletín Geológico - academia.edu
ABSTRACT A database containing 2547 earthquake focal mechanisms from Costa Rica,
southern Nicaragua, and northern Panama is analyzed to model the modern tectonic stress …
southern Nicaragua, and northern Panama is analyzed to model the modern tectonic stress …