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ESSD | Articles | Volume 10, issue 3
Earth Syst. Sci. Data, 10, 1503–1526, 2018
https://doi.org/10.5194/essd-10-1503-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Earth Syst. Sci. Data, 10, 1503–1526, 2018
https://doi.org/10.5194/essd-10-1503-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Review article 24 Aug 2018

Review article | 24 Aug 2018

Present-day surface deformation of the Alpine region inferred from geodetic techniques

Laura Sánchez et al.
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Altamimi, Z., Collilieux, X., and Métivier, L.: ITRF2008: an improved solution of the international terrestrial reference frame, J. Geodesy, 85, 457–473, https://doi.org/10.1007/s00190-011-0444-4, 2011. 
Altamimi, Z., Métivier, L., and Collilieux, X.: ITRF2008 plate motion model, J. Geophys. Res., 117, B07402, https://doi.org/10.1029/2011JB008930, 2012. 
Amante, C. and Eakins, B. W.: ETOPO1 Global Relief Model converted to PanMap layer format. NOAA-National Geophysical Data Center, PANGAEA, https://doi.org/10.1594/PANGAEA.769615, 2009. 
Aoudia, A., Amodio, A., Troisi, C., Manzino, A., Luchetta, A., Völksen, C., Drewes, H., Zivcic, M., Van der Voerd, J., Fosson, J. P., Carraro, C., Zampedri, G., Walpersdorf, A., Laffi, R., Fioroni, M., Barzaghi, R., Sabadini, R., Pasetti, L., and Sguero, D.: ALPS GPSQUAKENET. Alpine Integrated GPS Network: Real-Time Monitoring and Master Model for Continental Deformation and Earthquake Hazard, Intergared III B Project – Alpine Space, available at: http://www.alpine-space.org/2000-2006/uploads/media/ALPS-GPS_QUAKENET_Project_booklet.pdf (last access: 20 August 2018), 2007. 
Argnani, A.: Plate Tectonics and the Boundary between Alps and Apennines, Ital. J. Geosci., 128, 317–330, https://doi.org/10.3301/IJG.2009.128.2.317, 2009. 
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Short summary
We provide a surface-kinematics model for the Alpine region based on high-level data analysis of 300 geodetic stations continuously operating over 12.4 years. This model includes a deformation model, a continuous velocity field, and a strain field consistently assessed for the entire Alpine mountain belt. Horizontal and vertical motion patterns are clearly identified and supported by uncertainties better than ±0.2 mm a−1 and ±0.3 mm a−1 in the horizontal and vertical components, respectively.
We provide a surface-kinematics model for the Alpine region based on high-level data analysis of...
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