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.

We show that regional ocean modeling is necessary to resolve fine-scale dynamics that influence the efficiency of OAE. We highlight that global models, which may not resolve tides, submeso- to ...