| | [No title] (Site not responding. Last check: 2007-10-03) |
 | | Low frictional strength of faults is estimated based on existing models for earthquake recurrence, which account for compaction and hydrothermal lithification of fault rocks, as well as for the buildup of high fluid pressures in faults during interseismic periods. |
 | | In areas of elevated heat flow and for a geothermal gradient of 30°C/km, fault compaction, lithification, and changes in fluid pressure gradient are inferred to occur at shallow crustal depth (3 to 7 km). |
 | | On the basis of field evidence from many exhumed faults for lithification of fault gouge and for faulting at near-lithostatic fluid pressures, a modified crustal strength profile is suggested to represent the strength of many active faults which involve hydrothermal fluid flow. |
| www.agu.org /pubs/abs/jb/97JB01509/97JB01509.html (233 words) |