Scale-invariant stress orientations and seismicity rates near the San Andreas Fault

Geophysical Research Letters
By: , and 

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Abstract

We analyzed measurements of the direction of maximum horizontal compressive stress as a function of depth in two scientific research wells near the San Andreas Fault in central and southern California. We found that the stress orientations exhibit scale-invariant fluctuations over intervals from tens of cm to several km. Similarity between the scaling of the stress orientation fluctuations and the scaling of earthquake frequency with fault size suggests that these fluctuations are controlled by stress perturbations caused by slip on faults of various sizes in the critically-stressed crust adjacent to the fault. The apparent difference in stress scaling parameters between the two studies wells seem to correspond to differences in the earthquake magnitude-frequency statistics for the creeping versus locked sections of the fault along which these two wells are located. This suggests that stress heterogeneity adjacent to active faults like the San Andreas may reflect variations in stresses and loading conditions along the fault.

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Publication type Article
Publication Subtype Journal Article
Title Scale-invariant stress orientations and seismicity rates near the San Andreas Fault
Series title Geophysical Research Letters
DOI 10.1029/2010GL045025
Volume 37
Issue 24
Publication Date December 21, 2010
Year Published 2010
Language English
Publisher American Geophysical Union
Description L24304, 5 p.
Country United States
State California
Other Geospatial San Andreas Fault
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