Sands of the Tunisian shelf consist of a mixture in different proportions of bioclasts, generally prevalent, and quartz grains. Quartz is concentrated along shore lines, modern and ancient. Comparison of grain size analysed before and after acid treatment shows ; 1 ) an interaction between quartz and carbonate grains during transportation ; 2) that coastal sands are well sorted and clean ; 3) that sands of meadows range from well to poorly sorted and from clean to highly muddy ; 4) that neritic sediments deposited at present mostly consist of mud. Grain size analyses of bioclasts can be helpful in recognizing ancient environments.Passega R., Pitti C., Vittimberga P., Templeton R.S.M., Desprat R. C. - Granulométries et minéraux lourds / ...
Samples from sutface sediments of the shell, continental slope, and adjacent deep sea regions off We...
Foraminiferal studies in the gulf of Gab es show the effect of some environmental factors on the dis...
Sediments sampled in three lateral traverses from the outer continental shelf to the continental ris...
Sands of the Tunisian shelf consist of a mixture in different proportions of bioclasts, generally pr...
Microstructure and grain-size of the turbidity deposits in the Sidi Salem reservoir (Tunisia). The d...
The geochemical and grain size analysis were carried out on surface and down core sediments from the...
A sedimentological and mineralogical study of sedimentary cores allows reconstructing the evolution ...
International audienceThe authors report on two campaigns of high-resolution samplings along the sho...
This study aims to reconstruct the Holocene to modern depositional environments and the evolution o...
International audienceA very precise study of the heavy minerals of silty sands of Matmata Mounts (S...
International audienceIn the summer of 2015 the authors analysed grain size and surface sediment com...
Significant variations in the amount of carbonate and gypsum and also in the thickness of preserved ...
Twelve cores sampled in the siculo-tunisian area are studied with regard to sedimentology, grain-siz...
Exoscopy of quartz with the electron microscope allows definition of five grain types all originatin...
295-304Heavy mineral bearing beach sediments collected along a shore perpendicular transect between...
Samples from sutface sediments of the shell, continental slope, and adjacent deep sea regions off We...
Foraminiferal studies in the gulf of Gab es show the effect of some environmental factors on the dis...
Sediments sampled in three lateral traverses from the outer continental shelf to the continental ris...
Sands of the Tunisian shelf consist of a mixture in different proportions of bioclasts, generally pr...
Microstructure and grain-size of the turbidity deposits in the Sidi Salem reservoir (Tunisia). The d...
The geochemical and grain size analysis were carried out on surface and down core sediments from the...
A sedimentological and mineralogical study of sedimentary cores allows reconstructing the evolution ...
International audienceThe authors report on two campaigns of high-resolution samplings along the sho...
This study aims to reconstruct the Holocene to modern depositional environments and the evolution o...
International audienceA very precise study of the heavy minerals of silty sands of Matmata Mounts (S...
International audienceIn the summer of 2015 the authors analysed grain size and surface sediment com...
Significant variations in the amount of carbonate and gypsum and also in the thickness of preserved ...
Twelve cores sampled in the siculo-tunisian area are studied with regard to sedimentology, grain-siz...
Exoscopy of quartz with the electron microscope allows definition of five grain types all originatin...
295-304Heavy mineral bearing beach sediments collected along a shore perpendicular transect between...
Samples from sutface sediments of the shell, continental slope, and adjacent deep sea regions off We...
Foraminiferal studies in the gulf of Gab es show the effect of some environmental factors on the dis...
Sediments sampled in three lateral traverses from the outer continental shelf to the continental ris...