New GPS constraints on active deformation along the Africa-Iberia plate boundary
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...We did not find significant motion across the Pyrenees, as was reported by Asensio et al. [2012], and most of Iberia (except for the Betics in the south) [P erez-Pe~na et al., 2010; Koulali et al., 2011; de Lis Mancilla et al., 2013; Echeverria et al., 2013] thus moves with Eurasia....
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"New GPS constraints on active defor..." refers methods in this paper
...D by nodes and surface deformation due to locked faults during the interseismic period is modeled as due to dislocations in an elastic half-space (Okada, 1985)....
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...We use the program DEFNODE (McCaffrey, 2005), in which faults are represented in 3-D by nodes and surface deformation due to locked faults during the interseismic period is modeled as due to dislocations in an elastic half-space (Okada, 1985)....
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"New GPS constraints on active defor..." refers background in this paper
...…the position and velocity differences of selected sites with respect to a priori values defined by the IGS05 realization of the ITRF2005 reference frame (Altamimi et al., 2007) or an assumption of zero horizontal motion for 13 and 20 sites with respect to Eurasia or Africa (Nubia), respectively....
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