Seismicity and thermal structure along the northern San Andreas Fault system, California, USA

Kevin Patrick Furlong, Suzanne M. Atkinson

Research output: Contribution to journalArticle

8 Citations (Scopus)

Abstract

The correlation between depth patterns of seismicity and crustal thermal regime are investigated for the San Andreas Fault system. Regions of anomalous behavior include the occurrence of seismicity at temperatures (depths) substantially greater than or the cessation of seismicity at temperatures (depths) less than typical values observed in seismically active regions of the continents. Seismicity at temperatures significantly greater than target values indicate a need to re-evaluate the assumed geotherm and crustal lithology model. Regions where the seismicity cutoff is at temperatures significantly below target values are possible sites for the future occurrence of significantly deeper earthquakes than presently observed. Such sites need further study for analysis of possible increased earthquake risk. Comparisons of seismicity patterns with crustal thermal models may also provide a powerful tool in the evaluation of the patterns of heat production and thermal conductivity in heterogeneous continental crust.

Original languageEnglish (US)
Pages (from-to)23-30
Number of pages8
JournalTectonophysics
Volume217
Issue number1-2
DOIs
StatePublished - Jan 15 1993

Fingerprint

San Andreas Fault
thermal structure
seismicity
earthquakes
occurrences
temperature
lithology
continents
earthquake
crusts
thermal conductivity
cut-off
heat production
thermal regime
heat
conductivity
continental crust
evaluation

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth-Surface Processes

Cite this

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Seismicity and thermal structure along the northern San Andreas Fault system, California, USA. / Furlong, Kevin Patrick; Atkinson, Suzanne M.

In: Tectonophysics, Vol. 217, No. 1-2, 15.01.1993, p. 23-30.

Research output: Contribution to journalArticle

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