Zobrazeno 1 - 10
of 42
pro vyhledávání: '"Jamel, Touir"'
Publikováno v:
In Journal of African Earth Sciences June 2017 130:202-222
Publikováno v:
Carbonates and Evaporites. 37
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4201a8735dd9561bb7e99371a1327807
https://doi.org/10.1007/s13146-021-00744-3
https://doi.org/10.1007/s13146-021-00744-3
Publikováno v:
Stratigraphy. 16:265-277
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::813dc9884c528868ecb4bcf78f69ce7f
https://doi.org/10.29041/strat.16.4.265-277
https://doi.org/10.29041/strat.16.4.265-277
Publikováno v:
Carbonates and Evaporites. 34:1489-1509
Detailed analysis of the Chouabine Formation exposed in the western part of the Gafsa basin, southern Tunisia shows the presence of six principal facies. Vertical and lateral evolution of facies showed a gradual transition from intertidal to circatid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b60faaed2212941258f8a17de65c68ee
https://doi.org/10.1007/s13146-019-00498-z
https://doi.org/10.1007/s13146-019-00498-z
Publikováno v:
Journal of African Earth Sciences. 150:757-766
The field study and the petrographic observations of the limestone samples particularly from the Boukehil section allowthe identificationof four carbonate facies: (1) calcisphere-rich mudstone-wackestone, (2) Conglomeratic limestone, (3) bioclastic w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbcea931661d9536e4dc033ff32a6df6
https://doi.org/10.1016/j.jafrearsci.2018.10.004
https://doi.org/10.1016/j.jafrearsci.2018.10.004
Publikováno v:
Arabian Journal of Geosciences. 14
The Upper Valanginian–Hauterivian Meloussi Formation outcropping in Central Tunisia includes alternating sandstones, dolostones, and marls that developed within a paleodeltaic system. The present work aims to characterize the dolomites and interpre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f60a14fda9fb199dd2cf24aa0a488b34
https://doi.org/10.1007/s12517-021-07730-y
https://doi.org/10.1007/s12517-021-07730-y
Publikováno v:
Carbonates and Evaporites. 35
Based on their facies characteristics and stratal geometries, the carbonate deposits of the Middle Eocene outcropping in the Tamerza area (Western Gafsa Basin) led to the recognition of nine facies that were deposited in shallow marine environment su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a79c2960c5e4b19020866067b9de97a
https://doi.org/10.1007/s13146-020-00593-6
https://doi.org/10.1007/s13146-020-00593-6
Publikováno v:
Carbonates and Evaporites. 33:835-860
The Albian series have been deposited on both sides of a major E–W paleogeographic fault, which was inherited in the early stages of the Tethyan-rifting phase. To the south of this fault, a shallow platform domain (footwall block or horst) occurred
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02ed56730871f8b2a5aa8e66e75a111d
https://doi.org/10.1007/s13146-018-0451-0
https://doi.org/10.1007/s13146-018-0451-0
Publikováno v:
Carbonates and Evaporites. 34:893-908
Late Paleocene–Early Eocene deposits cropping out in Tamerza area were settled on a carbonate homoclinal ramp. Deposits which are ranged in six main facies record a gradual transition from intertidal to upper circatidal environment. Lateral variati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::904163b1fcc8b0b4eb582cca57b3d157
https://doi.org/10.1007/s13146-018-0424-3
https://doi.org/10.1007/s13146-018-0424-3
Publikováno v:
Journal of African Earth Sciences. 182:104284
The Berda Formation corresponds to an inner-shelf stratigraphic equivalent of the Campanian-Maastrichtian outer-shelf Abiod Formation of Tunisia. The present work aims to carry out a sedimentological study of the lower unit (Upper Campanian) of Berda
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2694f9d18f6f059a4e3a2446caeb2b6f
https://doi.org/10.1016/j.jafrearsci.2021.104284
https://doi.org/10.1016/j.jafrearsci.2021.104284