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GEOPHYSICAL RESEARCH LETTERS, VOL. 21, NO. 23, PAGES 2523–2526, 1994

3D Geometry of the Strain-Field at Transform Plate Boundaries: Implications for Seismic Rupture

P. Bodin

Center for Earthquake Research and Information, University of Memphis, Memphis, TN


R. Bilham

CIRES and Department of Geological Sciences, University of Colorado, Boulder, CO


Abstract

We examine the amplitude and distribution of slip on vertical frictionless faults in the zone of concentrated shear strain that is characteristic of transform plate boundaries. We study both a 2D and a 3D approximation to this strain field. Mean displacements on ruptures within the zone of concentrated shear strain are proportional to the shear strain at failure when they are short, and are limited by plate displacements since the last major earthquake when they are long. The transition between these two behaviors occurs when the length of the dislocation approaches twice the thickness of the seismogenic crust, approximately the breadth of the zone of concentrated shear strain observed geodetic ally at transform plate boundaries. This result explains the observed non-linear scaling relation between seismic moment and rupture length. A geometrical consequence of the 3D model, in which the strain-field tapers downward, is that moderate earthquakes with rupture lengths similar to the thickness of the crust tend to slip more at depth than near the surface. Seismic moments estimated from surface slip in moderate earthquakes (M≤7) will thus be underestimated. Shallow creep, if its along-strike dimension is extensive, can reduce a surface slip deficit that would otherwise develop on faults on which M<7 events are typical. In the absence of surface creep or other forms of off-fault deformation great earthquakes may be necessary features of transform boundaries with downward-tapering strain-fields.

Received 14 February 1994; accepted 9 August 1994.

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Citation: Bodin, P., and R. Bilham (1994), 3D Geometry of the Strain-Field at Transform Plate Boundaries: Implications for Seismic Rupture, Geophys. Res. Lett., 21(23), 2523–2526.