Genesis of Zn-Pb-(Ba-Sr) mineralization in the peridiapiric cover of Jebel El Akhouat, Ech Chehid salt dome, Northern Tunisia

2021 ◽  
Author(s):  
Nejib Jemmali ◽  
Larbi Rddad ◽  
Marta Sośnicka ◽  
Emna Rahali ◽  
Fouad Souissi ◽  
...  
Keyword(s):  
Salt Dome ◽  
Northern Tunisia

Plio-Quaternary Shortening Structures in Northern Tunisia

2018 ◽  
pp. 255-258
Author(s):  
Seifeddine Gaidi ◽  
Guillermo Booth-Rea ◽  
José Vicente Pérez ◽  
Fetheddine Melki ◽  
Wissem Marzougui ◽  
...  
Keyword(s):  
Northern Tunisia

Neogene tectonic evolution in Northern Tunisia: case of Chaouat-Mannouba area. Palaeoseismic event associated

2015 ◽  
Vol 8 (10) ◽  
pp. 8911-8925 ◽  
Author(s):  
Azizi Ramzi ◽  
Kadri Ali ◽  
Chihi Lassaad
Keyword(s):  
Tectonic Evolution ◽  
Northern Tunisia

Potentiality of clay raw materials from Gram area (Northern Tunisia) in the ceramic industry

2015 ◽  
Vol 112-113 ◽  
pp. 1-9 ◽  
Author(s):  
Faten Hammami-Ben Zaied ◽  
Riadh Abidi ◽  
Najet Slim-Shimi ◽  
Alireza K. Somarin
Keyword(s):  
Ceramic Industry ◽  
Raw Materials ◽  
Northern Tunisia

GRAVITY AND MAGNETIC INVESTIGATIONS AT THE GRAND SALINE SALT DOME, VAN ZANDT CO., TEXAS

Geophysics ◽  
1945 ◽  
Vol 10 (3) ◽  
pp. 376-393 ◽  
Author(s):  
Jack W. Peters ◽  
Albert F. Dugan
Keyword(s):  
Physical Properties ◽  
Quantitative Evaluation ◽  
Gravity Data ◽  
Salt Dome ◽  
Salt Mine ◽  
Geological Data ◽  
East Texas ◽  
Additional Information ◽  
Theoretical Mass ◽  
Gravity And Magnetic

During May, 1944, detailed gravity and magnetic surveys were made at the Grand Saline Salt Dome to secure additional information on the physical properties of this typical East Texas salt dome. The results of the surface gravity and magnetic surveys, and the subsurface gravity survey in the Morton Salt Mine are illustrated and discussed. Densities and the available subsurface data were compiled and were utilized in a quantitative evaluation of the observed gravity data. The theoretical mass distribution which was determined by this quantitative evaluation is not intended to represent the unique solution of the geophysical and geological data; instead, it is offered as a possible solution based on relatively simple assumptions.

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