Improving deformation models by discounting transient signals in geodetic data: 2. Geodetic data, stress directions, and long-term strain rates in Italy
Author:
Affiliation:
1. Istituto Nazionale di Geofisica e Vulcanologia; Sezione di Sismologia e Tettonofisica; L'Aquila Italy
2. Department of Earth, Planetary and Space Sciences; University of California; Los Angeles California USA
Funder
MIUR-FIRB “Abruzzo”
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016JB013038/fullpdf
Reference127 articles.
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3. Paired deformation sources of the Campi Flegrei caldera (Italy) required by recent (1980-2010) deformation history;Amoruso;J. Geophys. Res. Solid Earth,2014a
4. Clues to the cause of the 2011-2013 Campi Flegrei caldera unrest, Italy, from continuous GPS data;Amoruso;Geophys. Res. Lett.,2014b
5. The Pliocene-Pleistocene stratigraphic and tectonic evolution of the central sector of the Western Periadriatic Basin of Italy;Artoni;Mar. Pet. Geol.,2013
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