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Topic: Aseismic creep


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In the News (Fri 27 Nov 09)

  
  San Andreas Fault - Wikipedia, the free encyclopedia
The central segment of the San Andreas fault runs in a northwestern direction from Parkfield to Hollister.
While the southern section of the fault and the parts through Parkfield experience earthquakes, the rest of the central section of the fault exhibits a phenomenon called aseismic creep.
This results in the fault being able to move without the need of earthquakes.
en.wikipedia.org /wiki/San_Andreas_fault   (1394 words)

  
 USGS Earthquake Hazards Program » Glossary
It is sometimes called "seismic creep" to distinguish it from the slumping of rock or soil on slopes (which is also known as creep).
It is sometimes called "aseismic creep", since it does not trigger events greater than microearthquakes.
Creep is only known to occur on strike-slip faults.
earthquake.usgs.gov /regional/qfaults/glossary.php   (4638 words)

  
 UCLA - Earth and Space Sciences - Didier Sornette, Scientific Prediction of Catastrophies: A New Approach
We thus explored how the SOC concept can help understand the observed earthquake clustering on relatively narrow fault domains and the phenomenon of induced seismicity by human activity such as water impoundment in artificial lakes, gas and ore extraction.
We found that both pore pressure changes and mass transfers leading to incremental deviatoric stresses of less than 10 atmospheric pressure are sufficient to trigger seismic instabilities in the uppermost crust with magnitude ranging up to $7$ in otherwise historically aseismic areas.
We argued that these observations are in accord with the SOC hypothesis as they show that a significant fraction of the crust is not far from instability and can thus be made unstable by minute perturbations.
www.ess.ucla.edu /faculty/sornette/catastrophies.asp   (10272 words)

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