Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Rached Lakhdar"'
Publikováno v:
Journal of Petroleum Exploration and Production Technology, Vol 9, Iss 2, Pp 1007-1022 (2018)
Abstract The Bir M’Cherga basin (North-east Tunisia), with about 600 km2 area, had recorded four Middle Cretaceous source rocks well stratigraphically correlated with the four known oceanic anoxic sub-events: OAE1a, OAE1b, OAE1c, and OAE1d. Variety
Externí odkaz:
https://doaj.org/article/c017f24572b348c9a514b5eee1983c71
Publikováno v:
Journal of Petroleum Exploration and Production Technology, Vol 9, Iss 2, Pp 1023-1024 (2018)
In the original publication, article title has been incorrectly published as “Aptian–Albian oil shale unconventional system as registration of Cretaceous oceanic anoxic sub-events in the southern Tethys (Bir M’Cherga basin, Tunisia)” instead
Externí odkaz:
https://doaj.org/article/e76ca20ed393485d904209a9c4592fe7
Publikováno v:
Quaternary Research. 100:77-97
On the southeastern Tunisian coastline, very diverse living microbial mats colonize the lower supratidal and intertidal zones, and locally may extend into the upper infratidal zone. The interaction between the benthic cyanobacteria and their silicicl
Autor:
Rached, Lakhdar, Rachida, Talbi, Mohamed, Soussi, Younès, Jedoui, Sahbi, Jaouadi, Marco, Anzidei
Publikováno v:
Arabian Journal of Geosciences; May2022, Vol. 15 Issue 10, p1-20, 20p
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:
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
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 241:177-191
The Holocene sedimentary record of Sabkha Boujmel (SE Tunisia) is expressed by a shallowing-upward carbonate lagoon–tidal flat cycle (2.3 m thick) unconformably overlying continental silt–sandy sediment, Late Wurmian in age. The sedimentary packa
Autor:
Mohamed Soussi, Rached Lakhdar
Publikováno v:
Edition 1, Hammamet, Tunisie.
Resume : L’etude sedimentologique concerne des depots holocenes enfouis dans l’actuelle sebkha Boujmel comprenant des sables detritiques et/ou carbonates gypsiferes, des vases riches en matiere organique et des boues blanchâtres riches en carbon