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- W3033361262 abstract "aquifer geometry behavior in alluvial plains was confronted by lateral heterogeneity of the sandy bodies of the channels, alluvial fans, as well as other phenomenon occurring in the shallow marine environment and/or deep-water.The hydrogeological and litho-stratigraphic techniques, based on a spatial-temporal correlation of lithological units and cycles, lead to imprecisions on the system multilayered aquifers geometry and boundary conditions.This study appraises multi-source methods, which aim to overcome the constraints imposed by such a complex geometry approach. This method consists of combining hydrogeological boreholes (lithology), well logs, and geophysics data (Vertical Electric Surveys).For that, the integration of electrical data (300 VES) combined with well-logging records and hydrogeological boreholes (80 boreholes) in a GIS is used to establish a 3D model of the plio-quaternary deposits along the central part of the Rharb basin commonly known as The Sidi Yahia-Sidi Slimane sub-basin.The main results obtained show that above the ondular top of the Miocene-Pliocene marly substratum, appears four geoelectric intervals of variable thicknesses and extensions. Resistant or conductive lenticular forms truncate these intervals. Furthermore, the effect of deep structures on the establishment of these deposits is added.In the present work, the approach applied to the central Rharb sub-basin opens up great perspectives for the study of alluvial basins same as the Rharb basin." @default.
- W3033361262 created "2020-06-12" @default.
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- W3033361262 date "2020-03-11" @default.
- W3033361262 modified "2023-09-25" @default.
- W3033361262 title "Three-Dimensional Modeling of Plio-Quaternary Deposits of the Alluvial Sub-Basin of the Rharb (Sidi Yahya Sidi Slimne Sub-Basin-Morocco NW)" @default.
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- W3033361262 doi "https://doi.org/10.1145/3399205.3399245" @default.
- W3033361262 hasPublicationYear "2020" @default.
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