2011
DOI: 10.1016/j.jappgeo.2011.05.007
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Interpretation of magnetic data in the Sinop area of Mid Black Sea, Turkey, using tilt derivative, Euler deconvolution, and discrete wavelet transform

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Cited by 62 publications
(29 citation statements)
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“…Further, these images visually interpreted and digitized available magnetic breaks. Intersection of magnetic breaks and faults are marked for groundwater potential zones [13]. The magnetic breaks further spatially correlated with the existing lineament (major fault) for validation and confirmation.…”
Section: Methodsmentioning
confidence: 82%
“…Further, these images visually interpreted and digitized available magnetic breaks. Intersection of magnetic breaks and faults are marked for groundwater potential zones [13]. The magnetic breaks further spatially correlated with the existing lineament (major fault) for validation and confirmation.…”
Section: Methodsmentioning
confidence: 82%
“…The TDR also provides an automatic-gain-control filter which tends to equalize the response from both weak and strong anomalies (Verduzco et al, 2004). The half-distance between ±/4 contours provides an estimate of the source depth for vertical contacts or the distance between zero and +/4 or −/4 contour obtained from the TDR corresponds to the depth to the top of the vertical contact model (Salem et al, 2007;Oruc and Keskinsezer, 2008;Oruc and Selim, 2011).…”
Section: Methodsmentioning
confidence: 99%
“…Euler 3D deconvolution was employed to estimate the position of the structural lineaments in the study area from Bouguer data. The main objective of the Euler 3D deconvolution is to represent the geological structures that cause the gravity or magnetic anomalies using a 2D grid (Oruç and Selim, 2011).…”
Section: Gravity and 3d Euler Deconvolution Interpretationmentioning
confidence: 99%