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- W2619663136 abstract "We present the crustal deformation field in the Ibe rian Peninsula and northern Morocco, based on the analysis of the continuous GPS (CGPS) observations for the last five years, combined with the survey style observations (SGPS) of the CuaTeNeo network in eastern Betics. The analyzed CGPS stations come from several national and regional GNSS networks, with variable monument design and stability. Four CuaTeNeo campaigns were conducted with approximately a 4-year interval from 1997 to 2011. Although the calculated deformation field is comple x, some expected features could be easily identified. Considering the Eurasia fixed frame, th e highest velocities, as expected, are observed in Morocco, where the velocities reach 4.7±0.2 mm/yr. In southern Spain, stations located west of Almeria exhibit a westerly trend of motion, which r each 3.2±0.1 mm/yr at station SFER. The direction of these vectors makes us think that the main drivi ng force behind the observed deformations cannot be solely attributed to the Africa-Eurasia converge nce, but it should be due to the deeper geodynamic processes related to the subduction of the Betic-Al boran slab." @default.
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- W2619663136 date "2014-10-10" @default.
- W2619663136 modified "2023-09-26" @default.
- W2619663136 title "Present-day crustal deformation field of the Iberian Peninsula estimated by GPS measurements" @default.
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