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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:
Arabian Journal of Geosciences. 13
Magmatic events related to granodiorite and rhyodacite rocks in the Oued Belif area (NW Tunisia) are dated as 12.9 Ma and 8.3 Ma, respectively. These rocks are affected by a net fault system, veins, and breccias, attesting a post-magmatic hydrotherma
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
Publikováno v:
Arabian Journal of Geosciences. 11
Fe-ore and Pb-Zn (Ag) resources of Nefza region occur within hydrothermally altered sericite-schists and breccias, with Neogene molasse and lacustrine sediments and with a sequence of tertiary granodiorite-rhyodacite and basalts. Intrusions of interm