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Present-day deformation at plate boundary zones, recorded as GPS velocities, reflects the combination of plate motion and elastic strain accumulation. This suite of codes implements the block modeling methodology described by: Meade, B.J. and J.P. Loveless (2009), Block modeling with multiple fault network geometries and a linear elastic coupling estimator in spherical coordinates, Bulletin of the Seismological Society of America, 99(6), 3124–3139, doi:10.1785/0120090088.
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