Poster #089, San Andreas Fault System (SAFS)
A unified perspective of seismicity and fault coupling along the San Andreas Fault
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Poster Presentation
2021 SCEC Annual Meeting, Poster #089, SCEC Contribution #11496 VIEW PDF
emporal clustering, with repeating earthquakes as an end-member.
We compute a metric called the "fraction of background events", to describe relative dominance between aseismic and seismic processes. We show that this quantity is highly correlated (at a 93% level) with the rate of creep as measured from geodesy. The degree of fault coupling thus has a first-order effect on the long-term seismicity dynamics of the entire central San Andreas. Regions that exhibit a lower fraction of non-clustered background seismicity are interpreted as having a higher likelihood of triggering large mainshock-aftershock sequences by taking up an increasingly larger area of the fault surface via seismic slip.
Under this unified paradigm, the northwest ~75 km of the creeping segment may be more aptly described as a transition zone, with an increased likelihood of a rupture propagating through the entire ~150 km-long creeping segment. Our findings would be directly relevant to other fault systems globally.
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We compute a metric called the "fraction of background events", to describe relative dominance between aseismic and seismic processes. We show that this quantity is highly correlated (at a 93% level) with the rate of creep as measured from geodesy. The degree of fault coupling thus has a first-order effect on the long-term seismicity dynamics of the entire central San Andreas. Regions that exhibit a lower fraction of non-clustered background seismicity are interpreted as having a higher likelihood of triggering large mainshock-aftershock sequences by taking up an increasingly larger area of the fault surface via seismic slip.
Under this unified paradigm, the northwest ~75 km of the creeping segment may be more aptly described as a transition zone, with an increased likelihood of a rupture propagating through the entire ~150 km-long creeping segment. Our findings would be directly relevant to other fault systems globally.
SHOW MORE