The existence of observable precursory signals before large earthquakes has been debated for decades. Although observations preceding several large ea...

Slow-slip events (SSEs) release significant tectonic strain through aseismic slip and are observed at nearly every subduction zone across the globe. T...

Recent observations indicate that seismic rupture can migrate rapidly backwards, away from its advancing region, a phenomenon known as back-propagatin...

Understanding the dynamics of microearthquakes is a timely challenge to address current paradoxes in earthquake mechanics and to investigate earthquak...

A precise finite-fault model, including fault geometry and slip distribution, is essential for understanding the physics of an earthquake. However, co...

The Sumatran subduction zone is a highly seismic region, having produced several large earthquakes in the last decades. The accurate characterization ...

A key challenge in seismology is understanding why some seismic sequences develop into swarms without a mainshock, while others lead to a foreshock-ma...