A least-squares minimization approach to interpret gravity anomalies caused by a 2D thick, vertically faulted slab

We present a least-squares minimization approach to estimate simultaneously the depth to and thickness of a buried 2D thick, vertically faulted slab from gravity data using the sample spacing – curves method or simply s-curves method. The method also provides an estimate for the horizontal location...

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Main Authors: El-Sayed ABDELRAHMAN, Mohamed GOBASHY
Format: Article
Language:English
Published: Earth Science Institute, Slovak Academy of Sciences, Slovakia 2019-09-01
Series:Contributions to Geophysics and Geodesy
Subjects:
Online Access:https://journal.geo.sav.sk/cgg/article/view/204
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spelling doaj-3779a8bc49c64376b6f9c00366e31cfa2020-11-25T02:44:51ZengEarth Science Institute, Slovak Academy of Sciences, SlovakiaContributions to Geophysics and Geodesy1338-05402019-09-0149322924710.2478/congeo-2019-0012204A least-squares minimization approach to interpret gravity anomalies caused by a 2D thick, vertically faulted slabEl-Sayed ABDELRAHMAN0Mohamed GOBASHY1Geophysics Department, Faculty of Science, Cairo University, Giza, EgyptGeophysics Department, Faculty of Science, Cairo University, Giza, EgyptWe present a least-squares minimization approach to estimate simultaneously the depth to and thickness of a buried 2D thick, vertically faulted slab from gravity data using the sample spacing – curves method or simply s-curves method. The method also provides an estimate for the horizontal location of the fault and a least-squares estimate for the density contrast of the slab relative to the host. The method involves using a 2D thick vertical fault model convolved with the same finite difference second horizontal gradient filter as applied to the gravity data. The synthetic examples (noise-free and noise affected) are presented to illustrate our method. The test on the real data (Central Valley of Chile) and the obtained results were consistent with the available independent observations and the broader geological aspects of this region.https://journal.geo.sav.sk/cgg/article/view/204gravity thick fault, depth and thickness solutions, s-curves method, leastsquares method
collection DOAJ
language English
format Article
sources DOAJ
author El-Sayed ABDELRAHMAN
Mohamed GOBASHY
spellingShingle El-Sayed ABDELRAHMAN
Mohamed GOBASHY
A least-squares minimization approach to interpret gravity anomalies caused by a 2D thick, vertically faulted slab
Contributions to Geophysics and Geodesy
gravity thick fault, depth and thickness solutions, s-curves method, leastsquares method
author_facet El-Sayed ABDELRAHMAN
Mohamed GOBASHY
author_sort El-Sayed ABDELRAHMAN
title A least-squares minimization approach to interpret gravity anomalies caused by a 2D thick, vertically faulted slab
title_short A least-squares minimization approach to interpret gravity anomalies caused by a 2D thick, vertically faulted slab
title_full A least-squares minimization approach to interpret gravity anomalies caused by a 2D thick, vertically faulted slab
title_fullStr A least-squares minimization approach to interpret gravity anomalies caused by a 2D thick, vertically faulted slab
title_full_unstemmed A least-squares minimization approach to interpret gravity anomalies caused by a 2D thick, vertically faulted slab
title_sort least-squares minimization approach to interpret gravity anomalies caused by a 2d thick, vertically faulted slab
publisher Earth Science Institute, Slovak Academy of Sciences, Slovakia
series Contributions to Geophysics and Geodesy
issn 1338-0540
publishDate 2019-09-01
description We present a least-squares minimization approach to estimate simultaneously the depth to and thickness of a buried 2D thick, vertically faulted slab from gravity data using the sample spacing – curves method or simply s-curves method. The method also provides an estimate for the horizontal location of the fault and a least-squares estimate for the density contrast of the slab relative to the host. The method involves using a 2D thick vertical fault model convolved with the same finite difference second horizontal gradient filter as applied to the gravity data. The synthetic examples (noise-free and noise affected) are presented to illustrate our method. The test on the real data (Central Valley of Chile) and the obtained results were consistent with the available independent observations and the broader geological aspects of this region.
topic gravity thick fault, depth and thickness solutions, s-curves method, leastsquares method
url https://journal.geo.sav.sk/cgg/article/view/204
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