Geometry and evolution of the San Andreas fault zone in northern California

Kevin Patrick Furlong, W. D. Hugo, G. Zandt

Research output: Contribution to journalArticle

87 Citations (Scopus)

Abstract

The evolution of the San Andreas fault system is controlled by thermal-mechanical processes associated with the development and evolution of a narrow "slabless window' formed beneath the western edge of North America. This fault zone evolution begins after initiation of transform motion along the plate boundary with the northward migration of the Mendocino triple junction. As a consequence of initial lithospheric structure and the shallow emplacement of asthenospheric mantle, the plate boundary separating the North American and Pacific plates follows a complex three-dimensional geometry which varies through time. Seismic velocity structure, heat flow, seismicity, surface deformation, uplift, and fault development are controlled by the evolving thermal structure in the region after triple junction passage. Thermal-mechanical models have been used to evaluate the fault system's time-varying three-dimensional dynamical behavior, simulating the principal processes involved in the thermal-mechanical evolution of the San Andreas fault system. -from Authors

Original languageEnglish (US)
Pages (from-to)3100-3110
Number of pages11
JournalJournal of Geophysical Research
Volume94
Issue numberB3
DOIs
StatePublished - Jan 1 1989

Fingerprint

San Andreas Fault
fault zone
heat
geometry
Geometry
triple junction
plate boundary
lithospheric structure
North American plate
Time varying systems
Pacific plate
thermal structure
velocity structure
heat transmission
heat flow
overland flow
seismicity
emplacement
Earth mantle
transform

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Space and Planetary Science
  • Earth and Planetary Sciences (miscellaneous)
  • Palaeontology

Cite this

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Geometry and evolution of the San Andreas fault zone in northern California. / Furlong, Kevin Patrick; Hugo, W. D.; Zandt, G.

In: Journal of Geophysical Research, Vol. 94, No. B3, 01.01.1989, p. 3100-3110.

Research output: Contribution to journalArticle

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