RELATION FRACTURATION-MORPHOLOGIE IMPLICATIONS HYDROGEOLOGIQUES. EXEMPLE DES CALCAIRES FISSURES DE LA REGION DE CHERIA (NE ALGERIEN)

Please use this identifier to cite or link to this item: http://archives.univ-biskra.dz/handle/123456789/2886

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DC Field	Value	Language
dc.contributor.author	CHAMEKH K.	-
dc.contributor.author	BAALI F.	-
dc.contributor.author	YAHIAOUI A.	-
dc.contributor.author	DJABRI L.	-
dc.date.accessioned	2013-05-21T15:18:58Z	-
dc.date.available	2013-05-21T15:18:58Z	-
dc.date.issued	2013-05-21	-
dc.identifier.uri	http://archives.univ-biskra.dz/handle/123456789/2886	-
dc.description.abstract	The area of Chéria is located at Algerian, with 45 kilometers in the South-west of the town of Tébessa. The area catchment to study extends on a surface from 720 km2, shelters more than 74300 inhabitants and characterized by a semi-arid climate.The area is formed primarily by limestones of Maestrichtien and Eocene which are fissured karstic and which constitute the aquiferous potential of the area. This study tries to confirm the relations between morphology and the fracturing in limestones and to confront them with the flows of the tablecloths of the latter.	en_US
dc.language.iso	fr	en_US
dc.subject	Chéria, Tébessa, limestone, morphology, fracturing	en_US
dc.title	RELATION FRACTURATION-MORPHOLOGIE IMPLICATIONS HYDROGEOLOGIQUES. EXEMPLE DES CALCAIRES FISSURES DE LA REGION DE CHERIA (NE ALGERIEN)	en_US
dc.type	Article	en_US
Appears in Collections:	Journal N18

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