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Autor:
Ben Aissa Wiem, Véronique, Gardien, Ben Aissa Rania, Abdessalem, Ben Haj Amara, Said, Tlig, Ben Aissa Lassaad
Publikováno v:
Geology of Ore Deposits; Dec2023, Vol. 65 Issue 6, p625-643, 19p
Publikováno v:
Arabian Journal of Geosciences. 16
Publikováno v:
Arabian Journal of Geosciences. 14
The Chouichia ore deposits are one of the most important polymetallic Cu-Fe-rich mineralizations located in the front of the thrust zone of the Tunisian Tellian belt. This mineral occurrence is carried by veins and breccias hosted by the Upper Cretac
Publikováno v:
International Journal of Earth Sciences. 106:2653-2665
Hydrothermal ore deposits at Ain El Araâr-Oued Belif location are classified as epithermal deposits type. The ore bodies are hosted by upper Turonian (8–9 M.y) volcanic rhyodacitic complex. Polymetallic sulfide orebodies are mainly concentrated wi
Autor:
Said Tlig
Publikováno v:
Journal of African Earth Sciences. 118:324-327
Autor:
Said Tlig
Publikováno v:
Journal of African Earth Sciences. 110:100-115
The Upper Jurassic–Lower Cretaceous series in southern Tunisia and northwestern Libya are revisited in the light of fieldwork, facies patterns, biostratigraphy and wellbore data. Five megacycles delineated by major unconformities are described. The
Publikováno v:
Carbonates and Evaporites. 29:299-307
The El Ghine-Oum El Khialate sebkha extends in southeast Tunisia on over than 75 km2. This depression is filled by recent Quaternary deposits containing a brines aquifer situated at a depth varying from 1 to 10 m. This aquifer is highly rich in sodiu
Publikováno v:
AAPG Bulletin. 97:1051-1070
Jurassic deposition in the Maghrebian tethys was governed by eustasy and rifting. Two periods were delineated: (1) a carbonate shelf (Rhaetian–early Pliensbachian) and (2) a platform-basin complex (early Pliensbachian–Callovian). The carbonate sh
Publikováno v:
Journal of Petroleum Science and Engineering. :50-65
The sequence stratigraphy of the Lutetian–Langhian series in the Gulf of Gabes basin was defined using cuttings from 50 wells, wireline logs, biostratigraphic data and seismic data. The seismic profiles display a shallow inner shelf passing northea