PyLith

GNSS signals in South Korea after the 2011 Tohoku Earthquake
Quantify deformation rates in South Korea after the 2011 Tohoku Earthquake and find what their spatial distributions can be attributed to.
GNSS signals in South Korea after the 2011 Tohoku Earthquake
Subducted seamounts are strong asperities
The Daiichi-Kashima seamount subducted in the southern Japan trench is a strong asperity. Probably so are many other seamounts. Subducted seamounts functioning as a strong asperity can generate M7 earthquakes regularly (every ~20 years) and much larger tsunamigenic ones at a longer interval (100s of years).
Subducted seamounts are strong asperities
Sources of Stress in Intraplate Seismic Zones
Aims to estimate the magnitude of stress relevant to earthquake generation for intraplte seismic zones
Sources of Stress in Intraplate Seismic Zones
Effects of Preexisting Structures on the Seismicity of the Charlevoix Seismic Zone
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