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 …

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 …

Rupture‐zone averaged static stress drop in the 2011 M= 9 Tohoku‐Oki earthquake was
less than 5 MPa, but it caused a stress reversal in most of the offshore forearc, although the …

Inland Tohoku has been recognized as under the WNW-ESE compressional stress state
before the 2011 M9 Tohoku-Oki earthquake. Earthquakes that occurred there were …

A shallow M7. 3 event with a M6. 5 foreshock occurred along the Futagawa‐Hinagu fault
zone in Kyushu, SW Japan. We investigated the spatiotemporal variation of the stress …

On 6 February 2023, the M w 7.8 Kahramanmaraş, Türkiye, earthquake occurred on the East
Anatolian Fault Zone (EAFZ). This study examined the spatial variation of the stress field in …

The stress redistribution from an earthquake can produce localized measurable rotations of
the principal stress axes if the absolute level of differential stress in the crust is on the order …

Temporal variations of the fault frictional strength was investigated based on the diversity of
focal mechanisms in the source area of the Yamagata‐Fukushima border earthquake …

We investigated the induced seismicity, source mechanisms and mechanical responses of a
decametre-scale hydraulic stimulation of a pre-existing shear zone in crystalline rock, at the …

Tsunamis with amplitudes of up to 40 cm, related to the Mw 7.1 normal‐faulting earthquake
off Fukushima, Japan, on November 21, 2016, were clearly recorded by a new offshore wide …