Complex 3-D surface deformation in the 1971 San Fernando, California earthquake reveals static and dynamic controls on off-fault deformation

dc.contributor.authorGaudreau, É.
dc.contributor.authorHollingsworth, J.
dc.contributor.authorNissen, E.
dc.contributor.authorFunning, G. J.
dc.date.accessioned2024-03-05T23:01:03Z
dc.date.available2024-03-05T23:01:03Z
dc.date.issued2023
dc.description.abstractThe shallow 1971 MW 6.6 San Fernando, California earthquake involved a complex rupture process on an immature thrust fault with a non-planar geometry, and is notable for having a higher component of left-lateral surface slip than expected from seismic source models. We extract its 3-D coseismic surface displacement field from aerial stereo photographs and document the amount and width of the vertical and fault trace-parallel components of distributed deformation along strike. The results confirm the significant left-lateral surface offsets, suggesting a slip vector rotation at shallow depths. Comparing our offsets against field measurements of fault slip, we observe that most of the offset was accommodated in the damage zone, with off-fault deformation averaging 69% in both the fault trace-parallel and vertical components. However, the magnitude and width of off-fault deformation behave differently between the vertical and fault trace-parallel components, which, along with the rotation in rake near the surface, can be explained by dynamic rupture effects.
dc.description.reviewstatusReviewed
dc.description.scholarlevelFaculty
dc.description.sponsorshipE. G. was funded through an Alexander Graham Bell Canada Graduate Scholarship and Michael Smith Foreign Study Supplement from the Natural Sciences and Engineering Research Council of Canada, and a Montalbano Scholars Fellowship and President's Research Scholarship, both from University of Victoria. E. N. was supported by a Canada Research Chair and grants from the Natural Sciences and Engineering Research Council of Canada (NSERC Discovery Grant 2017-04029), the Canada Foundation for Innovation, and the BC Knowledge Development Fund. J.H. was supported by grants from CNES and BQR. G.F. was supported by SCEC Award 21128.
dc.identifier.citationGaudreau, É., Hollingsworth, J., Nissen, E., & Funning, G. J. (2023). Complex 3‐D surface deformation in the 1971 San Fernando, California earthquake reveals static and dynamic controls on off‐fault deformation. Journal of Geophysical Research: Solid Earth, 128(3). https://doi.org/10.1029/2022jb024985
dc.identifier.urihttps://doi.org/10.1029/2022jb024985
dc.identifier.urihttps://hdl.handle.net/1828/16045
dc.language.isoen
dc.publisherJournal of Geophysical Research: Solid Earth
dc.rightsAttribution-NonCommercial 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/
dc.subject.departmentSchool of Earth and Ocean Sciences
dc.titleComplex 3-D surface deformation in the 1971 San Fernando, California earthquake reveals static and dynamic controls on off-fault deformation
dc.typeArticle

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