Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Beya Mannai-Tayech"'
Publikováno v:
Arabian Journal of Geosciences. 14
This paper evaluates the Cenomanian-Turonian Bahloul Formation as a new target for an unconventional shale oil play in the Sahel Basin, eastern Tunisia to increase the oil supply. A detailed geochemical (Rock-Eval pyrolysis and biomarkers) and minera
Publikováno v:
Journal of African Earth Sciences. 129:944-959
2-D seismic reflection sections, borehole data as well as published and unpublished data have been investigated to reconstruct the paleogeography of southern Tunisia during Middle to Late Permian times. Paleogeographical reconstruction based on the i
Publikováno v:
Méditerranée
Méditerranée, Presses universitaires de Provence, 2015, pp.39-49. ⟨10.4000/mediterranee.7891⟩
Méditerranée, Presses universitaires de Provence, 2015, pp.39-49. ⟨10.4000/mediterranee.7891⟩
Une analyse palynologique a ete menee sur les depots de l’Holocene moyen et superieur ainsi que sur des echantillons de surface de la sebkha Boujmel. Les resultats preliminaires montrent une importante diversite vegetale et enregistrent les reponse
Autor:
Beya Mannai-Tayech, Nadia Ben Moktar
Publikováno v:
Arabian Journal of Geosciences. 8:11149-11159
The pollen analysis of the sedimentary series of marine origin outlines the environmental and climatic context of the Northeastern Tunisia during the Lower to Middle Miocene. The analysis of the pollen sequence reveals a changing climate: (1) a subtr
Publikováno v:
Comptes Rendus Geoscience. 345:251-261
The Messinian sediments of northeastern Tunisia were deposited under an active tectonic setting. They are organized in sequences indicating a transitional deposit from margin – littoral to lacustrine – continental facies. These series unconformab
Autor:
Nadia Ben Moktar, Beya Mannai-Tayech
Publikováno v:
Arabian Journal of Geosciences. 7:385-396
The Saouaf syncline is located in Tunisia Centre north-east, south-east of the Tunisian dorsal. The sedimentary series, starting with limestone and marlstone, is essentially an alternation of three terms, sandstone, clay and lignite. It is in this ba
Autor:
Sahbi Jaouadi, Laurent Dezileau, Nathalie Combourieu-Nebout, Giuseppe Siani, Nejib Kallel, Viviane Bout-Roumazeilles, Ridha Boussoffara, Rached Lakhdar, Beya Mannai-Tayech, Vincent Lebreton
Publikováno v:
Climate of the Past Discussions
Climate of the Past Discussions, European Geosciences Union (EGU), In press, ⟨10.5194/cp-2016-25⟩
Climate of the Past, Vol 12, Iss 6, Pp 1339-1359 (2016)
Climate of the Past
Climate of the Past, European Geosciences Union (EGU), 2016, 12 (6), pp.1339-1359. ⟨10.5194/cp-12-1339-2016⟩
Climate of the Past Discussions, 2016, ⟨10.5194/cp-2016-25⟩
Climate Of The Past (1814-9324) (Copernicus Gesellschaft Mbh), 2016, Vol. 12, N. 6, P. 1339-1359
Climate of the Past, 2016, 12 (6), pp.1339-1359. ⟨10.5194/cp-12-1339-2016⟩
Climate of the Past Discussions, European Geosciences Union (EGU), In press, ⟨10.5194/cp-2016-25⟩
Climate of the Past, Vol 12, Iss 6, Pp 1339-1359 (2016)
Climate of the Past
Climate of the Past, European Geosciences Union (EGU), 2016, 12 (6), pp.1339-1359. ⟨10.5194/cp-12-1339-2016⟩
Climate of the Past Discussions, 2016, ⟨10.5194/cp-2016-25⟩
Climate Of The Past (1814-9324) (Copernicus Gesellschaft Mbh), 2016, Vol. 12, N. 6, P. 1339-1359
Climate of the Past, 2016, 12 (6), pp.1339-1359. ⟨10.5194/cp-12-1339-2016⟩
Pollen and clay mineralogical analyses of a Holocene sequence from Sebkha Boujmel (southern Tunisia) trace the climatic and environmental dynamics in the lower arid bioclimatic zone over the last 8000 years. During the mid- to late Holocene transitio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c861eaee0e746d20c32e21780bda2076
https://doi.org/10.5194/cp-2016-25
https://doi.org/10.5194/cp-2016-25
Autor:
Jean-Pierre André, Beya Mannai-Tayech, Efterpi Koskeridou, Jean-Jacques Cornée, Pierre Moissette, Henriette Meon, Mohsen Rabhi
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology
Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 285 (1-2), pp.85-103. ⟨10.1016/j.palaeo.2009.10.028⟩
Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2010, 285 (1-2), pp.85-103. ⟨10.1016/j.palaeo.2009.10.028⟩
Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 285 (1-2), pp.85-103. ⟨10.1016/j.palaeo.2009.10.028⟩
Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2010, 285 (1-2), pp.85-103. ⟨10.1016/j.palaeo.2009.10.028⟩
International audience; The marine Messinian deposits of Tunisia cover a narrow littoral strip some 300 km long between the northern Bizerte and Cap Bon areas and the central-eastern Sahel region. Litho- and biofacies analysis of six stratigraphic se
Autor:
Beya Mannai-Tayech
Publikováno v:
Journal of African Earth Sciences. 54:53-61
In the Mediterranean region, the Miocene is a rather particular tectonic, eustatic and climatic epoch. In Tunisia, the complex distribution of the sedimentary sequences has been controlled by the interaction of these factors. These sequences are comp
Autor:
Beya Mannai-Tayech
Publikováno v:
Geobios. 39:71-84
Resume Durant le Miocene, le domaine atlasopelagien est soumis a un regime distensif et compressif evolutif, resultant des systemes de subduction–collision dus a la convergence des plaques africaine et eurasiatique. Ce regime se traduit par l'ouver