Linked from

The 11 pages that link to Pore pressure, each with the reason it gives.

• Effective stressRelated: Pore pressure reduces the portion of total stress carried by the solid framework.

• Induced seismicityRelated: Injected fluids can raise pressure in fault zones and reduce friction holding faults in place.

• CompactionRelated: Elevated pore pressure can support grain loads and slow compaction.

• Slow slip eventRelated: Fluid pressure changes effective fault friction and may influence slow-slip timing.

• Mantle viscosityRelated: Fluids can reduce effective stress and thereby change rock strength and apparent viscosity.

• Pore waterRelated: Pore-water pressure changes effective stress and can trigger sediment instability.

• Darcy's lawRelated: Differences in pore pressure drive flow through saturated porous media.

• CataclasiteRelated: Fluid pressure changes effective stress and therefore influences brittle faulting and cataclasite formation.

• Detachment faultRelated: Elevated fluid pressure can reduce effective stress and ease slip on low-angle surfaces.

• Brittle–ductile transition zoneRelated: It alters effective pressure and therefore the depth range of frictional failure.

• Byerlee's lawRelated: Elevated pore pressure lowers effective normal stress and therefore frictional strength.