Earthquakes can change the stress field in the Earth's lithosphere as they relieve and
redistribute stress. Earthquake‐induced stress changes have been observed as temporal …

Abstract The 2011 Mw 9.0 Tohoku‐oki earthquake is one of the world's best‐recorded
ruptures. In the aftermath of this devastating event, it is important to learn from the complete …

An Mw 6.2 earthquake occurred in Suzu, northeastern Noto Peninsula, Japan, on 5 May
2023, followed by many aftershocks. Before this mainshock‐aftershock sequence, an …

The hypothesis that the brittle–ductile transition (BDT) drastically reduces permeability
implies that potentially exploitable geothermal resources (permeability> 10− 16 m2) …

Hydrothermal activity and seismicity are abundant along the Yushu-Ganzi-Xianshuihe fault
system (YGXFS) in the eastern Tibetan Plateau. However, the processes and factors that …

Recent seismic and geodetic observations suggest the involvement of pressurized fluid and
aseismic slip during earthquake swarms. However, the interaction between these two factors …

Hydraulic fracturing experiments were conducted at 200–450° C by injecting water into
cylindrical granite samples containing a borehole at an initial effective confining pressure of …

This study describes an ongoing intense earthquake swarm in the crust of the northeastern
Noto Peninsula, Japan, that began around the end of 2019. Fluid movement related to …

The spatiotemporal distributions of hypocenters and temporal change in seismicity patterns
were investigated in details for events in the Yamagata‐Fukushima border earthquake …

In this study, we investigated temporal variations in stress drop and b‐value in the
earthquake swarm that occurred at the Yamagata‐Fukushima border, NE Japan, after the …