The San Andreas Fault Paleoseismic Record at Elizabeth Lake: Why are There Fewer Surface-Rupturing Earthquakes on the Mojave Section?

نویسندگان

چکیده

ABSTRACT The structural complexity of active faults and the stress release history along fault system may exert control on locus extent individual earthquake ruptures. Fault bends, in particular, are often invoked as a possible mechanism for terminating However, there few records available to examine how these factors influence along-fault recurrence earthquakes. We present new paleoearthquake chronology southern San Andreas at Elizabeth Lake integrate this record with existing timing frequency earthquakes vary through major restraining bend. This bend features mature, throughgoing right-lateral strike-slip fault, two intersections, proposed subsurface dip changes, >200 km long section misaligned regional plate motion. Frazier Mountain, Lake, Pallett Creek, Wrightwood, Pitman Canyon paleoseismic sites located relatively linear surface trace between bends. Our investigations document 4–5 earthquakes, since ?1100 C.E., similar number recorded Creek. In contrast, Mountain Wrightwood each 8–9 during same time period. Differences demonstrate that fewer rupture central portion than occur near bends intersections. Furthermore, similarity from Bidart Fan site northwest suggests broad, 30° curve Big Bend exerts less behavior 3D geometry Mojave sections fault.

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ژورنال

عنوان ژورنال: Bulletin of the Seismological Society of America

سال: 2021

ISSN: ['1943-3573', '0037-1106']

DOI: https://doi.org/10.1785/0120200218