The Miocene fluorite–schwazite–cinnabar veins at Jebel Oust dome, Zaghouan Fluorite District, Tunisia: fluid inclusions and evidence of mixing

Author:

Miladi Yasmine,Garnit Hechmi,Bouhlel Salah

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference110 articles.

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2. Anderson JE (1996) The Neogene structural evolution of the western margin of the Pelagian Platform. Central Tunisia. J Struct Geol 18:819–833

3. Appold MS, Garven G (1999) The hydrology of ore formation in the southeast Missouri district: numerical models of topography-driven fluid flow during the Ouachita orogeny: ECON. GEOL 94:913–935

4. Appold MS, Nunn JA (2005) Hydrology of the western Arkoma basin and Ozark platform during the Ouachita orogeny: implications for Mississippi Valley-type ore formation in the Tri-State Zn-Pb district: Geofluids 5:308–325

5. Bejaoui J (2012) Géologie, Minéralogie, Eléments en traces Inclusions Fluides, Isotopes et Modélisation Génétique des Gisements à Pb–Znet ou F, Ba de la Tunisie centro-septentrionale (Fedj Hassène, ElHamra, Ajered, El Kohol, Mecella, El Mokta et M’Tak). Thèse doct., Univ. Tunis II, pp 260

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