Carbonate accumulation and weathering of the granitic substratum of Tanecherfi Basin, northeastern Morocco

In the Tanecherfi Basin a granitic body is partly overlain by a calcrete, which only seems superimposed.Morphologically, the profiles consist of three horizons. The lowest one corresponds to a filling of carbonates into the weathered granitic rocks. Microscopically, the carbonates cut the primary minerals along open cracks and voids. In the second horizon, the increased carbonation results in calcite septa that gradually isolate rock cells inclosed in a micritic matrix forming a cortex. Gradually, the rock residues vanish and glaebules appear. The upper horizon is characterized by a micritic matrix associated with the disappearance of the nodules.These morphologic relations are confirmed by chemical data. The primary minerals are weathered: silica is locally released and precipitates partly around the glaebules; magnesium combines into the carbonate structure, but locally combines with the silica of the cortex of the glaebules. Aluminium seems to be totally removed.The granite-calcrete relationships indicate a weathering process rather to a simple superposition.