Abstract The Ain Allega, Mjar Hannech and Sidi Driss Pb‐Zn‐Ba‐Sr‐As‐(Hg) deposits in northern Tunisia are hosted in a post‐nappe anticline with a core of a Triassic evaporite diapir affected by the NE–SW‐trending Ghardimaou‐Cap Serrat and E‐W lineament. The ore minerals show different styles; particularly, impregnation in dolomite, cement of...
-
January 2022 (v1)Journal articleThe microbial controls on the deposition of Pb‐Zn minerals in carbonate‐hosted Tunisian ore depositsUploaded on: October 11, 2023
-
January 2022 (v1)Journal articleThe microbial controls on the deposition of Pb‐Zn minerals in carbonate‐hosted Tunisian ore deposits
International audience
Uploaded on: December 3, 2022 -
2022 (v1)Journal article
The Djebel El Hamra Pb-Zn-Ba-Sr (Hg) deposits in northern Tunisia are hosted in a post-nappe anticline with a core of a Triassicevaporite diapir affected by the NE–SW-trending Ghardimaou-Cap Serrat lineament. Three stages of mineralization occurred inthe Triassic dolostone: stages I and II caused alternating deposition of sulfate (Ba, Sr) and...
Uploaded on: December 4, 2022