Potential role of mantle-derived fluids in weakening the San Andreas Fault

Patrick M. Fulton, Demian Saffer

Research output: Contribution to journalArticle

42 Citations (Scopus)

Abstract

On the basis of both geomechanical and thermal data, the San Andreas Fault (SAF) has been interpreted to act as a weak plane within much stronger crust, allowing it to slip at very low shear stresses. One explanation for this weakness is that large fluid overpressures exist locally within the fault zone. However, mechanisms for generating, maintaining, and localizing pressures within the fault are poorly quantified. Here we evaluate whether realistic sources of mantle-derived fluids, proposed on the basis of high mantle helium signatures near the SAF, can generate localized fluid pressures within the fault zone in a manner consistent with a wide range of observations along the fault and in the San Andreas Fault Observatory at Depth borehole. We first calculate a reasonable estimate of the magnitude and location of a mantle-derived flux of water into the crust. This fluid flux results from dehydration of a serpentinized mantle wedge following the northward migration of the Mendocino Triple Junction and the transition from subduction to strike-slip tectonics. We then evaluate the potential effect of this water on fluid pressures within the crust using 2-D cross-sectional models of coupled fluid flow and heat transport. We show that in models with realistic permeability anisotropy, controlled by NE dipping faults and fractures within the country rock, large localized fluid pressures can be focused within a SAF acting as a hydrologic barrier. Our results illustrate a simple and potentially plausible means of weakening the SAF in a manner generally consistent with available hydrologic, thermal, and mechanical constraints.

Original languageEnglish (US)
Article numberB07408
JournalJournal of Geophysical Research: Solid Earth
Volume114
Issue number7
DOIs
StatePublished - Jul 4 2009

Fingerprint

San Andreas Fault
Earth mantle
fluid pressure
mantle
Fluids
fluid
fluids
crusts
crust
fault zone
slip
heat
overpressure
triple junction
Fluxes
Helium
country rock
boreholes
dipping
Water

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

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Potential role of mantle-derived fluids in weakening the San Andreas Fault. / Fulton, Patrick M.; Saffer, Demian.

In: Journal of Geophysical Research: Solid Earth, Vol. 114, No. 7, B07408, 04.07.2009.

Research output: Contribution to journalArticle

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