REVEL: A model for Recent plate velocities from space geodesy
By G. Sella, Timothy H. Dixon, A. Mao. 2002
1,161 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/674f1c5b8b1bd52caf8c1fcfc8686bba4e213876
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In Geophysics
- Thorsten W. Becker
- Clinton P. Conrad
- Mark D. Behn
- P. Silver
- Alireza Amiri-Simkooei
- A. Enns
- H. Schmeling
- Noel Gourmelen
Citations in the corpus
- Spatiotemporal filtering using principal component analysis and Karhunen-Loeve expansion approaches for regional GPS network analysis (2006, methodology): “Studies using CGPS measurements have revealed deformation patterns over a range of spatial scales from global plate motion [Larson et al., 1997; Sella et al., 2002; Prawirodirdjo and Bock, 2004] and geocenter motion [Blewitt et al., 2001; Dong et al., 2003] to regional crustal deformation at plate b”
- GPS constraints on Africa (Nubia) and Arabia plate motions (2003, methodology): “Estimates of presentday Euler vectors have been reported from an analysis of geodetic data by Larson et al. (1997) and Sella et al. (2002).”
- The dynamics of subduction and trench migration for viscosity stratification (2005, methodology): “From GPS measurements in the Andean region (Sella et al. 2002) one can estimate trench migration velocities of the Andean Trench of the order of 1 cm yr−1.”
- A four-dimensional viscoelastic deformation model for Long Valley Caldera, California, between 1995 and 2000 (2006, methodology): “In order to investigate local deformation from the GPS data, we removed the effects of the North American plate (NAP) rotation in the International Terrestrial Reference Frame (ITRF) 2000 (hNAP, /NAP, xNAP=4.598S, 82.918W, 0.1958/ma) following Sella et al. (2002).”
- Constraints on lithosphere net rotation and asthenospheric viscosity from global mantle flow models and seismic anisotropy (2010, background): “In fact, modern geodetic observations of plate motions [Sella et al., 2002; Kreemer et al., 2003] show nearly the same patterns and rates of relative motion as early characterizations [e.”
- Global mantle flow and the development of seismic anisotropy: Differences between the oceanic and continental upper mantle (2007, background): “By contrast, plate motions are thought to be steady or only gradually changing, except during times of plate reorganization [e.g., Engebretson et al., 1984], which is not thought to be occurring presently [e.g., Sella et al., 2002 ].”