Extreme multi-millennial slip rate variations on the Garlock fault, California: Strain super-cycles, potentially time-variable fault strength, and implications for system-level earthquake occurrence
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文摘

Multi-millennial, multi-earthquake strain super-cycles occur on the Garlock fault.

Super-cycles may coincide with temporal changes in elastic strain accumulation rate.

Variable strain accumulation rates may be tied to temporally variable fault strength.

Strain super cycle behavior precludes use of many probabilistic seismic hazard models.

A deeper understanding of earthquake occurrence requires system-level analysis.

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