Yuta Mitsui

Coseismic thermal pressurization can notably prolong earthquake recurrence intervals on weak rate and state friction faults: Numerical experiments using different constitutive equations

The Role of porosity evolution and fluid flow in frictional instabilities: A parametric study using a spring‐slider dynamic system

Fault instability on a finite and planar fault related to early phase of nucleation

Long-term slow slip events are not necessarily caused by high pore fluid pressure at the plate interface: an implication from two-dimensional model calculations

Interseismic pore compaction suppresses earthquake occurrence and causes faster apparent fault loading

Two-dimensional model calculations of earthquake cycle on a fluid-infiltrated plate interface at a subduction zone: Focal depth dependence on pore pressure conditions

Photographic evidence of luminescence during faulting in granite

Can we estimate fault instability from prior phase of nucleation

The Role of porosity evolution and fluid flow in frictional instabilities: A parametric study using a spring-slider dynamic system: POROSITY EVOLUTION AND DYNAMIC FRICTION

Interseismic pore compaction suppresses earthquake occurrences and unexpectedly promotes fault loading on model faults with loading by slip deficits