Costras carbonatadas en la sucesión aluvial distal eocena de la Formación Hamada de Boudenib II al sur del Alto Atlas (Marruecos)
- Armenteros, I. 1
- Ben Brahim, M. 2
- Blanco, J.A. 1
- Huerta, P. 1
- Suárez, M. 1
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1
Universidad de Salamanca
info
- 2 Mohammed 1st University, Marruecos
ISSN: 0213-683X
Año de publicación: 2003
Número: 34
Páginas: 199-202
Tipo: Artículo
Otras publicaciones en: Geogaceta
Resumen
On the southern edge of the High Atlas Mountains of Morocco, the Tertiary continental deposits form extensive tablelands, the so-called "Hamada", in the Boudenib area. Two units have been defined in the Paleogene: a Lower unit "Hamada de Boudenib I" (lower Eocene) and an Upper one "Hamada de Boudenib II" of Middle/Upper Eocene age. This latter lies unconformably and covers most of the Lower unit; generally dips towards the south and thickens in this same direction. Their central basin deposits essentially consist of mudstones and sandy mudstones, deposited in distal areas (alluvial plain) of alluvial fans with sparse channels and ephemeral carbonate ponding. Intense processes of crust formation produced several facies of calcretes and dolocretes and the ubiquitous palygorskite. The duricrust features indicate that they were formed by continuous processes of carbonate precipitation in the vadose and capillary zones of soil profiles, developed on the alluvial plain, with alternative wetting and drying episodes in a semiarid climate.