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TitleEffects of earthquake recurrence on localization of interseismic deformation around locked strike-slip faults
 
AuthorZhu, Y; Wang, KORCID logo; He, J
SourceJournal of Geophysical Research, Solid Earth vol. 125, issue 8, e2020JB019817, 2020 p. 1-15, https://doi.org/10.1029/2020JB019817
Image
Year2020
Alt SeriesNatural Resources Canada, Contribution Series 20200301
PublisherAmerican Geophysical Union
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf; html
Subjectstectonics; geophysics; structural geology; Science and Technology; Nature and Environment; seismology; bedrock geology; structural features; faults, strike-slip; shear zones; tectonic environments; deformation; earthquakes; seismicity; seismic risk; earthquake risk; geodynamics; models; rheology; stress analyses; modelling; satellite geodesy; cyclic processes
Illustrationsprofiles; geoscientific sketch maps; location maps; schematic representations; time series; tables
ProgramPublic Safety Geoscience Assessing Earthquake Geohazards
Released2020 06 30
AbstractLocalized geodetic deformation of arctan shape around locked strike-slip faults is widely reported, but there are also important exceptions showing distributed deformation. Understanding the controlling mechanism is important to hazard assessment and geodynamic analysis. Here we use simple finite element viscoelastic earthquake cycle models to investigate the basic mechanics of this process. Our models feature a vertical strike-slip fault in an elastic layer overlying a viscoelastic substrate of Maxwell or Burgers rheology, with or without a low-viscosity shear zone representing deeper extension of the fault. We demonstrate that the primary control on the localization of interseismic deformation is the recurrence interval of past earthquakes. Given viscosity, shorter recurrence leads to greater localization, regardless of the rheological model used. The presence of a low-viscosity deep fault does not change this conclusion, although it tends to lessen localization by promoting faster postseismic stress relaxation. Distributed deformation, although less reported, is a natural consequence of very long recurrence and in theory should be as common as localized deformation. We think that the apparent propensity of the latter is likely associated with the much greater quantity and better quality of geodetic observations from higher-rate and shorter-recurrence faults. Our results also show the important role of nearby earthquakes along the same fault. For faults of relatively short recurrence, frequent ruptures of nearby segments, modeled using a migrating rupture sequence, further enhances localization. For faults of very long recurrence, faster near-fault deformation induced by a recent earthquake may give a false impression of localized interseismic deformation.
Summary(Plain Language Summary, not published)
Geodetic monitoring of interseismic deformation is widely used as a tool to assist hazard assessment, but the physical process of the deformation and hence the meaning of the recorded geodetic signal is not well understood. It has become customary to infer greater earthquake potential from deformation that occurs near the fault (localization of deformation). In this work, using strike-slip faults as examples, we demonstrate that the degree of localization depends on the length of the characteristic earthquake recurrence interval of the specific fault. Deformation is more localized if the recurrence interval is shorter. The commonly used method thus needs revision by considering earthquake history and recurrence interval, all in a viscoelastic Earth model.
GEOSCAN ID326915

 
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