期刊名称:Science et changements planétaires / Sécheresse
印刷版ISSN:1147-7806
电子版ISSN:1777-5922
出版年度:2010
卷号:21
期号:4
页码:252-256
DOI:10.1684/sec.2010.0247
出版社:John Libbey Eurotext
摘要:Figures See all figures Authors Hicham Aqil , Driss Khattach , Radia El Gout , Abdenbi El Mandour , Olivier Kaufmann Université Mohammed Premier COSTE et laboratoire LGA Département de géologie Faculté des sciences 60000 Oujda Maroc, Université Cadi Ayyad Faculté des sciences Semlalia Département de géologie Avenue Prince Moulay Abdellah BP 511 40000 Marrakech Maroc, Faculté polytechnique de Mons Géologie rue Houdain, 9 7000 Mons Belgique Key words: aquifer, gravimetry, hydrogeology, Morocco, semiarid zone DOI : 10.1684/sec.2010.0247 Page(s) : 252-6 Published in: 2010 The purpose of the present work is to show the contribution of gravimetric data interpretation to surveying deep aquifers and to providing insights into the structure of the plains. We use as our example the Angad's plain, which is hydrogeologically very interesting. The gravimetric data interpretation, through the application of various techniques of filtering (horizontal derivative, upward continuation), along with the integration of borehole data made it possible to outline the structure of the Angad plain by showing its different units and the spatial organization of faults.
关键词:aquifer; gravimetry; hydrogeology; Morocco; semiarid zone