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 …

The shear force along convergent plate boundary faults (megathrusts) determines the height
of mountain ranges that can be mechanically sustained,,–. However, whether the true height …

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 …

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 …

In order to investigate the spatial distribution of the crustal stress state across NE Japan, we
determined 1370 focal mechanisms by picking P-wave polarities from seismograms …

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 …