The underlying mechanism of the ongoing seismic swarm in the Noto Peninsula, Japan,
which generates earthquakes at 10 times the average regional rate, remains elusive. We …

Documenting the interplay between slow deformation and seismic ruptures is essential to
understand the physics of earthquakes nucleation. However, slow deformation is often …

Tremor signals are weak and emergent, and the physics governing their generation is not
well understood. Here, I report on tremor occurring along the Dead Sea Transform (DST) …

Very low‐frequency earthquakes (VLFs) are characterized by longer source duration and
smaller stress drop than regular earthquakes of similar magnitude. Recent studies have …

We report the first catalog of low‐frequency earthquakes in the Hikurangi subduction zone,
located beneath the Kaimanawa Range of the North Island at 50 km depth, downdip of …

Laboratory acoustic emissions (AEs) serve as small-scale analogues to earthquakes,
offering fundamental insights into seismic processes. To ensure accurate physical …

Estimating the radiated energy of small‐to‐moderate (Mw< 5) earthquakes remains
challenging because their energy decay significantly during wave propagation. Even when …

Numerous efforts have been made to interpret the intriguing characteristics of low-frequency
earthquakes (LFEs) and tectonic tremor in relation to regular earthquakes. At subduction …

Hyuga-nada, off the Pacific coast of Kyushu along the Nankai Trough in southwest Japan, is
one of the most active slow earthquake regions around Japan. We estimated the energies of …