2018
DOI: 10.1016/j.jappgeo.2018.03.023
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Improving a maximum horizontal gradient algorithm to determine geological body boundaries and fault systems based on gravity data

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Cited by 17 publications
(1 citation statement)
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“…This method involves the calculation of a horizontal gradient and comparison of the horizontal gradient of a centre point with its eight nearest neighbours in four directions within each 3 × 3 calculation grid. The horizontal location and magnitude of the maximum values are found by interpolating a second‐order polynomial through the trio of points provided that the magnitude of the middle point is greater than its two nearest neighbours in one direction (Van Kha et al., 2018).…”
Section: Gravity Data Analysismentioning
confidence: 99%
“…This method involves the calculation of a horizontal gradient and comparison of the horizontal gradient of a centre point with its eight nearest neighbours in four directions within each 3 × 3 calculation grid. The horizontal location and magnitude of the maximum values are found by interpolating a second‐order polynomial through the trio of points provided that the magnitude of the middle point is greater than its two nearest neighbours in one direction (Van Kha et al., 2018).…”
Section: Gravity Data Analysismentioning
confidence: 99%