2021
DOI: 10.1007/s12040-020-01519-5
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Appraisal of Veldurti–Kalva–Gani (VKG) fault, Cuddapah Basin, India: Gravity and magnetic approach

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“…The identification of fault disruptions is a standard task for potential field geophysical methods. Faults, both dips and upthrows, which represent vertical displacements, are effectively distinguished by their gravitational and magnetic fields as gradient zones or zones with a change in field characteristics [7,8]. Lineaments for the identification of such zones can be accurately traced both manually and automatically based on the fields themselves or their transformations [9][10][11].…”
Section: Strike-slip Structures In Geophysical Datamentioning
confidence: 99%
“…The identification of fault disruptions is a standard task for potential field geophysical methods. Faults, both dips and upthrows, which represent vertical displacements, are effectively distinguished by their gravitational and magnetic fields as gradient zones or zones with a change in field characteristics [7,8]. Lineaments for the identification of such zones can be accurately traced both manually and automatically based on the fields themselves or their transformations [9][10][11].…”
Section: Strike-slip Structures In Geophysical Datamentioning
confidence: 99%