Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Ines Ezzine"'
Publikováno v:
Przegląd Naukowy Inżynieria i Kształtowanie Środowiska, Vol 28, Iss 4, Pp 547-556 (2019)
The industrial development of the outcrops in the Tunis-Zaghouane area could represent an important economic driver for the country. The main structures are introduced and illustrated with onsite field observations. Moreover, samples which were extra
Externí odkaz:
https://doaj.org/article/8f8188e0812546ac922c7f280603add0
Publikováno v:
Estudios Geologicos, Vol 68, Iss 2, Pp 165-177 (2012)
[fr] En Tunisie Centro-Septentrionale, la bordure septentrionale du fossé de Kalâat Khasba a été considéré comme une bordure d’effondrement à jeu normal, ayant fonctionnée du Crétacé inférieur jusqu’au Quaternaire. Une étude de terrai
Externí odkaz:
https://doaj.org/article/f4388727f5aa43dc9a0483a65366c9f8
Karst aquifers belong to the fractured aquifer family. The Zaghouan region located in NE of Tunisia (North Africa) is characterized by a high degree of karstification due to the climate impact and the development of fracture network. Survey using ele
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f9d0801c78ba8e41f2308f9e319bb17
https://doi.org/10.5194/egusphere-egu22-10251
https://doi.org/10.5194/egusphere-egu22-10251
Publikováno v:
Journal of Geology & Geophysics.
Apart from the Triassic salt bodies, there are several structural elements that characterize the Oued Zarga area. The new field data allowed us to deduce that the structural evolution of this region is essentially based on two generations of dextral
Publikováno v:
Estudios Geologicos, Vol 68, Iss 2, Pp 165-177 (2012)
In Central-northern Tunisia, the septentrional border of Kalâat Khasba trough was considered as a normal fault which has functioned since the Cretaceous to Quaternary periods. A stratigraphic and geophysical recent study of the Kalâat Khasba trough
Publikováno v:
Arabian Journal of Geosciences. 5:1117-1125
A residual anomaly gravity map of the Maktar area has been processed via several methods including horizontal gradient, upward continuation, and Euler deconvolution to highlight structures hidden by sedimentary cover. These methods reinforce the exis