2004
DOI: 10.1016/j.jog.2004.02.021
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Three-dimensional strain tensor estimation by GPS observations: methodological aspects and geophysical applications

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Cited by 48 publications
(12 citation statements)
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“…To solve this problem, the above fundamental mathematical model needs to be refined. In this research, based on Equations (4) and (6), when the elevation is 90 degrees and the measurement environment is ideal, the observation precision can be regarded as the only result of receiver noise to a great extent [27,43]. It leads to the basic relations:…”
Section: Of 18mentioning
confidence: 99%
“…To solve this problem, the above fundamental mathematical model needs to be refined. In this research, based on Equations (4) and (6), when the elevation is 90 degrees and the measurement environment is ideal, the observation precision can be regarded as the only result of receiver noise to a great extent [27,43]. It leads to the basic relations:…”
Section: Of 18mentioning
confidence: 99%
“…1). Several numerical methods exist to solve velocity gradient tensor, e.g., Delaunay triangulation (Calais et al 2002), or statistical selection of homogeneous field (Pietrantonio and Riguzzi 2004); here, we used a regularly spaced gridded interpolation, with the distance weighted approach (Shen et al 1996;Allmendinger et al 2007;Cardozo and Allmendinger 2009). We constructed a uniform grid (5 9 5 km) in the area of the investigations (i.e., southern Tyrrhenian Sea and surroundings), and we estimated strain and rotation rate components at the center of each cell, using all the GPS velocities.…”
Section: Gps Data Processing and Strain Rate Field Analysismentioning
confidence: 99%
“…The velocities of Area B are roughly convergent towards the 2002-2003 degassing area. The horizontal strain rate estimated by STRAINGPS software (Pietrantonio and Riguzzi 2004) of Area B is shown in Fig. 2d.…”
Section: Velocity and Strain Rate Fieldsmentioning
confidence: 99%