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...
Main Authors: | , |
---|---|
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 |
id |
doaj-3779a8bc49c64376b6f9c00366e31cfa |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT elsayedabdelrahman aleastsquaresminimizationapproachtointerpretgravityanomaliescausedbya2dthickverticallyfaultedslab AT mohamedgobashy aleastsquaresminimizationapproachtointerpretgravityanomaliescausedbya2dthickverticallyfaultedslab AT elsayedabdelrahman leastsquaresminimizationapproachtointerpretgravityanomaliescausedbya2dthickverticallyfaultedslab AT mohamedgobashy leastsquaresminimizationapproachtointerpretgravityanomaliescausedbya2dthickverticallyfaultedslab |
_version_ |
1724765606617546752 |