Contribution of gravimetry to the study of Triffa basin structure (north-eastern Morocco): hydrogeological implications.

Contribution of gravimetry to the study of Triffa basin structure (north-eastern Morocco): hydrogeological implications. Various techniques (horizontal and vertical derivatives, upward continuation, Euler deconvolution) have been applied to the gravity data from the Triffa's plain and the north flank of the Beni-Snassen massif to delineate various major geological structures such as faults and basins. These results allow the production of a structural map showing the fault systems for the survey area. This map forms the basis for planning future hydrogeological research in this region. To cite this article: D. Khattach et al., C R. Geoscience 336 (2004). (C) 2004 Academie des sciences. Publie par Elsevier SAS. Tous droits reserves.