Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Zayneb, Amri"'
Publikováno v:
In Proceedings of the Geologists' Association February 2018 129(1):40-56
Publikováno v:
HAL
Arabian Journal of Geosciences
Arabian Journal of Geosciences, 2021, 15 (12), ⟨10.1007/s12517-021-09266-7⟩
Arabian Journal of Geosciences
Arabian Journal of Geosciences, 2021, 15 (12), ⟨10.1007/s12517-021-09266-7⟩
International audience; The Cretaceous outcrops of Borj Cedria-Bou Kournine area belongs to the NE-trending Atlas system of northern Tunisia. This area exposes sub-meridian folds associated with numerous N-to NWtrending major fault systems. This stud
Publikováno v:
Journal of African Earth Sciences
Journal of African Earth Sciences, 2020, 170, pp.103876. ⟨10.1016/j.jafrearsci.2020.103876⟩
Journal of African Earth Sciences, Elsevier, 2020, 170, pp.103876. ⟨10.1016/j.jafrearsci.2020.103876⟩
Journal of African Earth Sciences, 2020, 170, pp.103876. ⟨10.1016/j.jafrearsci.2020.103876⟩
Journal of African Earth Sciences, Elsevier, 2020, 170, pp.103876. ⟨10.1016/j.jafrearsci.2020.103876⟩
International audience; Surface and subsurface data are used to illustrate the halokinetic style, structural evolution and kinematics of the Lansarine–Baouala salt structure in the Alpine domain of Tunisia. It corresponds to a salt structure showin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9d27476e5658a6fd46b2aa157623404a
https://hal.science/hal-02979179/document
https://hal.science/hal-02979179/document
Publikováno v:
Journal of Structural Geology
Journal of Structural Geology, 2022, 154, ⟨10.1016/j.jsg.2021.104501⟩
Journal of Structural Geology, 2022, 154, ⟨10.1016/j.jsg.2021.104501⟩
International audience; Wide variety of salt structures –from typical diapirs to large allochthonous salt sheets– are recognized in the Northern Tunisian Atlas. In this study, we present for the first time the presence of a diapiric structure, Bi
Publikováno v:
Arabian Journal of Geosciences. 11
New stratigraphic data, lithostratigraphic correlations, and fault kinematic analysis are used to discuss the basin geometry and sedimentation patterns of the northeastern Tunisia during Cretaceous times. Significant facies and thickness variations a