Second Vertical Derivative

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Gravity/Magnetic GlossaryDownload this dictionary
Second Vertical Derivative
A second vertical derivative map of a potential field may be calculated by application of a frequency domain or space domain filter to a potential field grid file. The result is an anomaly enhancement or residual map related to the "curvature" of the input field. Inflection points on the anomalies of the input field will be zero values on the derivative map and may have special interpretation significance.

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