NDLI: Contribution Des Isotopes De L'environnement Pour La Comprehension Du Fonctionnement De L' Aquifere Mio-plioquaternaire Du Haouz De Marrakech (maroc)

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Contribution Des Isotopes De L'environnement Pour La Comprehension Du Fonctionnement De L' Aquifere Mio-plioquaternaire Du Haouz De Marrakech (maroc)

Content Provider	Semantic Scholar
Author	Abourida, A. Errouane, S. Bahir, Mohammed Silva, Marlos Cheggour, A.
Copyright Year	2004
Abstract	The study area «Haouz plain» is Located at the center of Morocco, it extend on a sur face of 2800 km 2 , limited by the Jbilet hilIs in the North, the High-Atlas range in the South, R' dat wadi in the East and the Essaouira-Chichaoua plateau in the West. The area climate is semi-arid, characterized by low precipitations varying between 160 mm/year and 250mm/year and important variation in temperature between the winter and the summer with respectively 5°C and 45°C. Its hydrographic network is represented by the Tensift system which receives alI the affluents of central and Westem Haouz. These affluents are characterized by weak flows with important seasonal variations. The Haouz plain is a sedimentary basin, being along the northem edge of the high atlas, it presents a geologic succession going from the primary to the recent Quatemary. The mio-plioquatemary formations, stemming from the dismantling of the atlasic chain, refuge an important and generalized water table on alI the plain. This water table shows very vari able hydrodynamic characteristics, reflecting the complexity of the deep structures of the plain, 1986) and also the lithological variability of the mio-plioquatemary formations.
Starting Page	161
Ending Page	167
Page Count	7
File Format	PDF HTM / HTML
DOI	10.3989/egeol.04603-692
Volume Number	60
Alternate Webpage(s)	http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/download/92/88
Alternate Webpage(s)	https://doi.org/10.3989/egeol.04603-692
Language	English
Access Restriction	Open
Content Type	Text
Resource Type	Article

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