Analysis and Interpretation of the Field and Laboratory Geophysical Measurements of Black-Sand Beach Deposits, East Rosetta, Egypt

The present study deals with the analysis and interpretation of the results of field geophysical survey and laboratory geophysical measurements. The study of the magnetic and electrical methods was selected because the beach sands contain many minerals that have magnetic and electric properties. Ana...

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Main Authors: Mohamed A. El-Sadek, Ahmed A. Ammar, Sayed A. Elkhateeb
Format: Article
Language:English
Published: Wiley 2012-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2012/435216
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author Mohamed A. El-Sadek
Ahmed A. Ammar
Sayed A. Elkhateeb
author_facet Mohamed A. El-Sadek
Ahmed A. Ammar
Sayed A. Elkhateeb
author_sort Mohamed A. El-Sadek
collection DOAJ
description The present study deals with the analysis and interpretation of the results of field geophysical survey and laboratory geophysical measurements. The study of the magnetic and electrical methods was selected because the beach sands contain many minerals that have magnetic and electric properties. Analysis and interpretation of the field and laboratory magnetic and geoelectric maps demonstrated that the investigated beach-alluvial deposits can be subdivided according to their magnetic and geoelectric properties into three main zones striking nearly parallel to the shoreline of the Mediterranean Sea at the study area. The northern zone is more enriched in black sands than the central or southern zones. Field and laboratory magnetic susceptibility measurements provided very useful maps for the concentration of heavy minerals. The deep-seated magnetic response was calculated at an average depth of 239.6 m, while the near-surface magnetic responses were computed at average depths of 9.1, 57.9, and 81.8 m, respectively. The correlation between the geophysical features, recorded on the total magnetic field intensity, the electric resistivity, the IP chargeability, and the calculated metal factor, was found to agree to a great extent. The heavymineral concentration was found to decrease with depth. However, the heavyminerals show parallel zones below the surface, suggesting similar sedimentation environments.
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issn 1687-885X
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spelling doaj-art-ac1fbe69257b4399b1804afbb045aa8d2025-08-20T02:20:22ZengWileyInternational Journal of Geophysics1687-885X1687-88682012-01-01201210.1155/2012/435216435216Analysis and Interpretation of the Field and Laboratory Geophysical Measurements of Black-Sand Beach Deposits, East Rosetta, EgyptMohamed A. El-Sadek0Ahmed A. Ammar1Sayed A. Elkhateeb2Exploration Division, Nuclear Materials Authority, P.O. Box 530, Maadi, Cairo, EgyptExploration Division, Nuclear Materials Authority, P.O. Box 530, Maadi, Cairo, EgyptExploration Division, Nuclear Materials Authority, P.O. Box 530, Maadi, Cairo, EgyptThe present study deals with the analysis and interpretation of the results of field geophysical survey and laboratory geophysical measurements. The study of the magnetic and electrical methods was selected because the beach sands contain many minerals that have magnetic and electric properties. Analysis and interpretation of the field and laboratory magnetic and geoelectric maps demonstrated that the investigated beach-alluvial deposits can be subdivided according to their magnetic and geoelectric properties into three main zones striking nearly parallel to the shoreline of the Mediterranean Sea at the study area. The northern zone is more enriched in black sands than the central or southern zones. Field and laboratory magnetic susceptibility measurements provided very useful maps for the concentration of heavy minerals. The deep-seated magnetic response was calculated at an average depth of 239.6 m, while the near-surface magnetic responses were computed at average depths of 9.1, 57.9, and 81.8 m, respectively. The correlation between the geophysical features, recorded on the total magnetic field intensity, the electric resistivity, the IP chargeability, and the calculated metal factor, was found to agree to a great extent. The heavymineral concentration was found to decrease with depth. However, the heavyminerals show parallel zones below the surface, suggesting similar sedimentation environments.http://dx.doi.org/10.1155/2012/435216
spellingShingle Mohamed A. El-Sadek
Ahmed A. Ammar
Sayed A. Elkhateeb
Analysis and Interpretation of the Field and Laboratory Geophysical Measurements of Black-Sand Beach Deposits, East Rosetta, Egypt
International Journal of Geophysics
title Analysis and Interpretation of the Field and Laboratory Geophysical Measurements of Black-Sand Beach Deposits, East Rosetta, Egypt
title_full Analysis and Interpretation of the Field and Laboratory Geophysical Measurements of Black-Sand Beach Deposits, East Rosetta, Egypt
title_fullStr Analysis and Interpretation of the Field and Laboratory Geophysical Measurements of Black-Sand Beach Deposits, East Rosetta, Egypt
title_full_unstemmed Analysis and Interpretation of the Field and Laboratory Geophysical Measurements of Black-Sand Beach Deposits, East Rosetta, Egypt
title_short Analysis and Interpretation of the Field and Laboratory Geophysical Measurements of Black-Sand Beach Deposits, East Rosetta, Egypt
title_sort analysis and interpretation of the field and laboratory geophysical measurements of black sand beach deposits east rosetta egypt
url http://dx.doi.org/10.1155/2012/435216
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AT ahmedaammar analysisandinterpretationofthefieldandlaboratorygeophysicalmeasurementsofblacksandbeachdepositseastrosettaegypt
AT sayedaelkhateeb analysisandinterpretationofthefieldandlaboratorygeophysicalmeasurementsofblacksandbeachdepositseastrosettaegypt