Dynamic triggering of earthquakes by seismic waves is a robustly observed phenomenon
with well-documented examples from over 30 major earthquakes. We are now in a position …

Natural soil CO 2 emissions constitute a substantial portion of the carbon emitted in the
atmosphere, particularly in volcano-tectonic areas where deep CO 2 supply is also present …

Earthquakes occur in clusters or sequences that arise from complex triggering mechanisms,
but direct measurement of the slow subsurface slip responsible for delayed triggering is …

Large earthquakes trigger very small earthquakes globally during passage of the seismic
waves and during the following several hours to days,,,,,,,,,, but so far remote aftershocks of …

We determined earthquake locations through re-picking of P-and S-wave arrival times
recorded by BMKG network. Earthquake locations were determined using Hypoellipse code …

An M s 6.4 earthquake struck Yangbi County in western Yunnan province, China, on 21 May
2021, causing damage in the nearby region. Intensive foreshock activity started three days …

The deep extension of the San Andreas Fault is believed to be cree**, but the recent
observations of tectonic tremors from these depths indicate a complex deformation style. In …

Aftershocks region have been extensively reported to expand logarithmically with time. The
associated migration velocity is typically of the order of several km/decade but can be much …

Low‐frequency earthquakes (LFEs) are small, rapidly recurring slip events that occur on the
deep extensions of some major faults. Their collective activation is often observed as a …

Geothermal/volcanic regions are most susceptible to local earthquake triggering by regional
and remote earthquakes. Transient stresses caused by surface waves of these earthquakes …