In fault gouge, fluids drive chemical healing by cementing grains, a mechanism for seismic slip in rocks frictionally ...

By modeling dehydration-driven fluid pressure, a new study links deep fluids to where megathrust earthquakes end and slow slip begins.

Oceanic transform faults are strike-slip boundaries—faults that move horizontally rather than up and down and connect offset ...

Cardiovascular diseases remain a leading cause of mortality globally, driving the need for more precise diagnostic and predictive tools. Traditional ...