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Touissit, Touissit District, Oujda-Angad Province, Oriental Region, Morocco
This locality features lead-zinc deposits replacing dolomite.The Pb–Zn mineralisation took place in dolomite strata by ascending hot, saline fluids probably during the Late Jurassic. Fluid inclusion data indicate that the mineralisation occurred at ambient condition of 100–135 °C and pressures of 150–200 bar.
Mineral List
Mineral list contains entries from the region specified including sub-localities53 entries listed. 30 valid minerals.
Localities in this Region
Morocco
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References
- Claveau, Paulhac & Pellerin (1952)
- Mineral. Rec. 15:347-350
- Mineral. Rec. 18:430
- Mineral. Rec. 20:69
- Mineral. Rec. 20(5): 396
- Rocks & Min.: 65:27
- - Bouabdellah, M., Fontboté, L. Haeberlin, Y., Llinares, L., Leach., D., Spangenberg, J. (1999): Zoned sulphur isotope signatures at the Mississippi Valley-type Touissit - Bou Beker - El Abed District (Morocco-Algeria) - Evidence for thermochemical sulphate reduction and mixing of sulphur sources. In: C.J. Stanley et al. (eds.), Mineral deposits: processes to processing, Proceedings of the 5th biennial SGA meeting, London, England, 22-25 August 1999, p. 821-824. http://www.unige.ch/sciences/terre/mineral/publications/onlinepub/bouabdellah_sga99_touissit.pdf
- S. Makhoukhi et al. (2000): Modelling of an MVT deposit: Touissit-Bou Beker district (eastern Morocco). Journal of Geochemical Exploration 69-70, 109-113.
- S. Makhoukhi et al. (2003): Aqueous and hydrocarbon inclusions in dolomite fromTouissit-Bou Beker district, Eastern Morocco: a Jurassic carbonate hosted Pb-Zn (Cu) deposit. Journal of Geochemical Exploration 78-79 (Proceedings of Geofluids IV), 545–551. (Abstract)
- Mineral. Rec. 15:347-350
- Mineral. Rec. 18:430
- Mineral. Rec. 20:69
- Mineral. Rec. 20(5): 396
- Rocks & Min.: 65:27
- - Bouabdellah, M., Fontboté, L. Haeberlin, Y., Llinares, L., Leach., D., Spangenberg, J. (1999): Zoned sulphur isotope signatures at the Mississippi Valley-type Touissit - Bou Beker - El Abed District (Morocco-Algeria) - Evidence for thermochemical sulphate reduction and mixing of sulphur sources. In: C.J. Stanley et al. (eds.), Mineral deposits: processes to processing, Proceedings of the 5th biennial SGA meeting, London, England, 22-25 August 1999, p. 821-824. http://www.unige.ch/sciences/terre/mineral/publications/onlinepub/bouabdellah_sga99_touissit.pdf
- S. Makhoukhi et al. (2000): Modelling of an MVT deposit: Touissit-Bou Beker district (eastern Morocco). Journal of Geochemical Exploration 69-70, 109-113.
- S. Makhoukhi et al. (2003): Aqueous and hydrocarbon inclusions in dolomite fromTouissit-Bou Beker district, Eastern Morocco: a Jurassic carbonate hosted Pb-Zn (Cu) deposit. Journal of Geochemical Exploration 78-79 (Proceedings of Geofluids IV), 545–551. (Abstract)
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Locality Updated: Wheal Coates, St Agnes, St Agnes District, Cornwall, England, UKFrom David Ifold, 19th Jun 2013 22:44:10
















