Time filter

Source Type

Gafsa, Tunisia

Henchiri M.,Sidi Ahmed Zarrouk | Fattah N.,Company of Phosphates of Gafsa
Arabian Journal of Geosciences

Sedimentary biogenic silica from Redeyef in Gafsa basin (southern Tunisia) was analysed for its 29Si and 27Al magic angle spinning nuclear magnetic resonance (MAS NMR) spectra and complemented by X-ray diffraction and SEM observations. The 29Si MAS NMR spectrum is characterized by the abundance of hydroxylated silicon, displayed in resonance intensities and reflects a clear tendency towards dissolution of diatomaceous amorphous silica and the occurrence of the hydrated silica, which is the main component that ensures the diagenetic transition via the mechanism of dissolution-precipitation to other more crystalline silica phases, after the lost of its hydroxyls groups (water) by heating (burial). 27Al MAS NMR reveals two coordinations of Al; the octahedrally coordinated Al suggests the presence of clay relics trapped during crystal growth or a microcrystalline zeolite (clinoptilolite detected by SEM observations), while the tetrahedrally coordinated Al suggests the presence of minor quantities of minerals with tetrahedral Al, such as an Al-rich fluid and/or minerals such as feldspars. © 2013 Saudi Society for Geosciences. Source

Henchiri M.,Sidi Ahmed Zarrouk | Abidi R.,Al Manar II | Jemmali N.,Sidi Ahmed Zarrouk
Arabian Journal of Geosciences

The Triassic salt diapirs in central Tunisia show splendid large multicoloured crystals of quartz. The study of these crystals and their host rocks sheds light on their origin and, more specifically, the relationships between silica authigenesis and its host rocks. Petrographic analyses of quartz crystals show strongly undulose euhedral to subeuhedral crystals (generally rhombohedral crystals) with concentration of many solid inclusions including sulphates and dolomite. Voids, shelter pores and negative crystals of gypsum, anhydrite and dolomite rhombs are found near the central parts of the crystals. Preserved anhydrite inclusions and dissolved evaporite are also found in these crystals. XRD analyses of white and black quartz crystals show crystalline alpha-quartz as the only silica phase present in most samples with a crystallinity index of 5. Accessory minerals include small relict patches of unreplaced calcite, gypsum, dolomite and anhydrite that escaped replacement. Fourier transform infrared (FTIR) spectra reveal the presence of abundant sulphate and organic compound included in the silica masses. The quartz crystals occurring in the allochthonous Triassic salt bodies are typically authigenic owing to the euhedral shape, the absence of any siliciclastic grains in the host rocks of quartz crystals, and also, to the absence of any sedimentary, wind or water-induced controls on the crystal distribution in their hosting rocks. Quartz growth in Triassic salt diapirs is a complex multistage and possibly continuous mechanism. During the progressive uplift of Triassic evaporites and dolomites, the dissolution of evaporites is enhanced and creates pores for the precipitation of the silica with development of larger quartz crystals. The colour variability in the quartz is ascribed to different ambient materials or fluids during crystallization. Remnant organic matter, before being altered and oxidised, could likely be included in the silica masses of the quartz and may serve not only to catalyse the precipitation and the growth but also to darken the quartz as well. Silica necessary for the formation of the quartz is mainly derived from two potential sources: (1) the presence of green and red clays in the Triassic salts and (2) silica-rich diagenetic fluids percolating from adjacent Lower Cretaceous sandy aquifers. © 2015, Saudi Society for Geosciences. Source

Discover hidden collaborations