Abstract The 2011 March 11 Tohoku-oki great (Mw 9.1) earthquake ruptured the plate
boundary megathrust fault offshore of northern Honshu with estimates of shallow slip of 50 m …

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 frictional resistance on a fault during slip controls earthquake dynamics. Friction
dissipates heat during an earthquake; therefore, the fault temperature after an earthquake …

The mechanics of great subduction earthquakes are influenced by the frictional properties,
structure, and composition of the plate-boundary fault. We present observations of the …

Episodic tremor and slow slip (ETS) occurs in the transition zone between the locked
seismogenic zone and the deeper, stably sliding zone. Actual mechanisms of ETS are …

В монографии приведены результаты многолетних исследований закономерностей
деформирования нарушений сплошности массивов горных пород. На основе …

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 …

摘要2008 年汶川地震后, 为查明北京地区现今地应力状态, 评价断裂稳定性,
相继在北京地区开展了5 个深孔(600~ 1000m) 的水压致裂法地应力测量 …

Fault slip during plate boundary earthquakes releases a portion of the shear stress
accumulated due to frictional resistance to relative plate motions. Investigation of 101 large …

Earthquakes occur by overcoming fault friction; therefore, quantifying fault resistance is
central to earthquake physics. Values for both static and dynamic friction are required, and …