An optimal multiscale approach to interpret gravity data using successive decomposition of the Bouguer anomaly
A multiscale interpretive approach is presented to identify multiscale discontinuities and sources boundaries, and to obtain comprehensive pseudo-section density images of 2D structures at depth. This interpretive approach is based on the total horizontal gradient and apparent density operator appli...
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Earth Science Institute, Slovak Academy of Sciences, Slovakia
2018-06-01
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Online Access: | https://journal.geo.sav.sk/cgg/article/view/180 |
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doaj-a850a49bd50548c291d1757be091b1a72020-11-25T03:38:32ZengEarth Science Institute, Slovak Academy of Sciences, SlovakiaContributions to Geophysics and Geodesy1338-05402018-06-0148213316010.2478/congeo-2018-0005180An optimal multiscale approach to interpret gravity data using successive decomposition of the Bouguer anomalyMohamed ARFAOUI0Mohamed Hedi INOUBLI1Adnen AMIRI2Office National des Mines, 24, Rue de l’Energie, 2035, La Charguia, Tunis, TunisiaUniversité Tunis-El Manar, Faculté des Sciences de TunisUniversité Tunis-El Manar, Faculté des Sciences de Tunis, TunisiaA multiscale interpretive approach is presented to identify multiscale discontinuities and sources boundaries, and to obtain comprehensive pseudo-section density images of 2D structures at depth. This interpretive approach is based on the total horizontal gradient and apparent density operator applied to the gravity anomalies of pseudo-depth slices derived from the successive decomposition of the Bouguer anomaly. This approach is applied to gravity data from the northwestern part of Tunisia, it provides the fault system repartition at different depths and describes the density distribution within the basins and trough. Thus, the NW–SE and NE–SW faults are the deepest whereas the N–S and E–W faults are relatively superficial. The density pseudo-sections reveal the vertical continuity of salt Triassic outcrops of Jebel Debadib as well as a diapiric model,the presence of a Triassic salt dome in the Kalaa El Khasba through and dense series under the Miopliocene and Quaternary deposits of the Mejarda basin.https://journal.geo.sav.sk/cgg/article/view/180gravity anomalies, tunisia, multiscale discontinuities, pseudo-depth slices, pseudo-section density |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Mohamed ARFAOUI Mohamed Hedi INOUBLI Adnen AMIRI |
spellingShingle |
Mohamed ARFAOUI Mohamed Hedi INOUBLI Adnen AMIRI An optimal multiscale approach to interpret gravity data using successive decomposition of the Bouguer anomaly Contributions to Geophysics and Geodesy gravity anomalies, tunisia, multiscale discontinuities, pseudo-depth slices, pseudo-section density |
author_facet |
Mohamed ARFAOUI Mohamed Hedi INOUBLI Adnen AMIRI |
author_sort |
Mohamed ARFAOUI |
title |
An optimal multiscale approach to interpret gravity data using successive decomposition of the Bouguer anomaly |
title_short |
An optimal multiscale approach to interpret gravity data using successive decomposition of the Bouguer anomaly |
title_full |
An optimal multiscale approach to interpret gravity data using successive decomposition of the Bouguer anomaly |
title_fullStr |
An optimal multiscale approach to interpret gravity data using successive decomposition of the Bouguer anomaly |
title_full_unstemmed |
An optimal multiscale approach to interpret gravity data using successive decomposition of the Bouguer anomaly |
title_sort |
optimal multiscale approach to interpret gravity data using successive decomposition of the bouguer anomaly |
publisher |
Earth Science Institute, Slovak Academy of Sciences, Slovakia |
series |
Contributions to Geophysics and Geodesy |
issn |
1338-0540 |
publishDate |
2018-06-01 |
description |
A multiscale interpretive approach is presented to identify multiscale discontinuities and sources boundaries, and to obtain comprehensive pseudo-section density images of 2D structures at depth. This interpretive approach is based on the total horizontal gradient and apparent density operator applied to the gravity anomalies of pseudo-depth slices derived from the successive decomposition of the Bouguer anomaly. This approach is applied to gravity data from the northwestern part of Tunisia, it provides the fault system repartition at different depths and describes the density distribution within the basins and trough. Thus, the NW–SE and NE–SW faults are the deepest whereas the N–S and E–W faults are relatively superficial. The density pseudo-sections reveal the vertical continuity of salt Triassic outcrops of Jebel Debadib as well as a diapiric model,the presence of a Triassic salt dome in the Kalaa El Khasba through and dense series under the Miopliocene and Quaternary deposits of the Mejarda basin. |
topic |
gravity anomalies, tunisia, multiscale discontinuities, pseudo-depth slices, pseudo-section density |
url |
https://journal.geo.sav.sk/cgg/article/view/180 |
work_keys_str_mv |
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