2019
DOI: 10.2478/congeo-2019-0007
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A new method for complete quantitative interpretation of gravity data due to dipping faults

Abstract: We have developed a simple method to determine completely the model parameters of a buried dipping fault from gravity data (depths to the centers of the upper and lower portions of the faulted thin slab, dip angle, and amplitude coefficient). The method is based on defining the anomaly values at the origin and at four symmetrical points around the origin on the gravity anomaly profile. By defining these five pieces of information, the dip angle is determined for each value of the depth of the lower portion of … Show more

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Cited by 7 publications
(9 citation statements)
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“…The mismatch between the estimated anomaly using the suggested method and that using Abdelrahman et al. (2019), may be due to that the second method is highly affected by presence of different nearby structures and/or noise.…”
Section: Application Of Pso Approach To Gazelle Fault Egypt Field Exmentioning
confidence: 93%
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“…The mismatch between the estimated anomaly using the suggested method and that using Abdelrahman et al. (2019), may be due to that the second method is highly affected by presence of different nearby structures and/or noise.…”
Section: Application Of Pso Approach To Gazelle Fault Egypt Field Exmentioning
confidence: 93%
“…The gravity anomaly results from a profile taken normal to dipping fault can be expressed by (Abdelrahman et al., 2013; Abdelrahman et al., 2019; Essa, 2013; Telford et al. 1976): g(xi,z,w,θ)=M(π+tan1(xix0z+cotθ)tan1(xix0w+cotθ))i=1,2,3,4,N, where xi is the horizontal location, z is the depth to the center of the upper part of the layer, w is the depth to the center of the lower part of the layer, x0 is the origin (Figure 1) and M is the amplitude factor (=2GΔ σ h) related to thickness ( h ), G is the gravitational constant, and Δ σ is the density contrast.…”
Section: Methodsmentioning
confidence: 99%
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