2015
DOI: 10.1117/12.2204828
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Research on matching area selection based on multiple features fusion of full tensor gravity gradient

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Cited by 3 publications
(4 citation statements)
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“…(g(i, j + 1) + g(i + 1, j + 1) − g(i, j) − g(i + 1, j), σ s represents the standard deviation of the slope, S represents the slope of the gravity field,S φ is the slope in the latitudinal direction, S λ is the slope in the longitudinal direction, scGrid is the grid side length, and S is the average slope in the calculation window. (11) To calculate the gravity anomaly difference entropy, the formula is as follows:…”
Section: Gravity Field Feature Parametersmentioning
confidence: 99%
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“…(g(i, j + 1) + g(i + 1, j + 1) − g(i, j) − g(i + 1, j), σ s represents the standard deviation of the slope, S represents the slope of the gravity field,S φ is the slope in the latitudinal direction, S λ is the slope in the longitudinal direction, scGrid is the grid side length, and S is the average slope in the calculation window. (11) To calculate the gravity anomaly difference entropy, the formula is as follows:…”
Section: Gravity Field Feature Parametersmentioning
confidence: 99%
“…Due to the close correlation between the calibration results of the suitable areas and the selection of the starting point, in order to make the calibration results more accurate, we selected three starting points for trajectory matching on four equal differences in each direction. The starting point for the east-west heading was (3500,3500), (3500,7500), (3500,1150); the starting point for the northeast heading was (3000,3000), (3000,4600), (3000,6200); the starting point for the north-south heading was (3500,3500), (7500,3500), (11,500,3500); and the starting point for the northwest heading was (9000,3000), (9000,4600), (9000,6200). In the experiment, all the suitable areas for trajectory matching calibration from three starting points were considered to be suitable.…”
Section: Validation and Application Of The New Gravity Field Feature ...mentioning
confidence: 99%
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“…The local standard deviation, local energy, local entropy, roughness, slope, and correlation coefficient parameters were mainly used. The threshold of local standard deviation and local entropy was obtained by the experimental method, which was used as the selection criterion of the suitable area [8]. In 2016, based on the theory of fractal geometry, Bo Wang et al proposed the isotropic coefficient by analyzing the spectral characteristics of the three-dimensional surface gravity anomaly sequence.…”
Section: Introductionmentioning
confidence: 99%