 | Choulet, Flavien, Barbanson, Luc, Buatier, Martine, Richard, James, Vennemann, Torsten, Ennaciri, Aomar, Zouhair, Mohamed (2017) Characterization and origin of low-T willemite (Zn2SiO4) mineralization: the case of the Bou Arhous deposit (High Atlas, Morocco) Mineralium Deposita, 52 (7) 1085-1102 doi:10.1007/s00126-016-0675-7 | Journal (article/letter/editorial) | | mineralization: the case of the Bou Arhous deposit (High Atlas, Morocco) Choulet Flavien 1 & Barbanson...mineral in the carbonate-hosted Bou Arhous zinc deposit. This deposit is located in the High Atlas intracontinental...Lausanne, Switzerland 4 Managem Group, Casablanca, Morocco hydrothermal fluids. The formation of the High...contribution of silicate minerals of the host limestone, hydrothermal fluids probably transported Si and...Non-sulfide zinc ore deposit . Cathodoluminescence . Germanium . Stable isotopes . Morocco Introduction Unconventional |  | Choulet, F., Buatier, M., Barbanson, L., Guégan, R., Ennaciri, A. (2016) Zinc-rich clays in supergene non-sulfide zinc deposits. Mineralium Deposita, 51 (4) 467-490 doi:10.1007/s00126-015-0618-8 | Journal (article/letter/editorial) | | understood. With the example of the Bou Arhous Zn-Pb ore deposit in the Moroccan High Atlas, this study...Orléans, France 3 Groupe Managem, Casablanca, Morocco and formation of interstratified zinc clay minerals...Supergene zinc deposits . Karst . Clay minerals . Morocco Introduction Clays are often considered to be...successful applications in Namibia, Peru, and Morocco. Supergene non-sulfide zinc deposits are formed...different genetic types may occur together in a given deposit, affecting the texture of ores and providing an |  | Bouabdellah, Mohammed, Boukirou, Wissale, Potra, Adriana, Melchiorre, Erik, Bouzahzah, Hassan, Yans, Johan, Zaid, Khadra, Idbaroud, Mohammed, Poot, Julien, Dekoninck, Augustin, Levresse, Gilles (2021) Origin of the Moroccan Touissit-Bou Beker and Jbel Bou Dahar Supergene Non-Sulfide Biomineralization and Its Relevance to Microbiological Activity, Late Miocene Uplift and Climate Changes. Minerals, 11 (4) 401 doi:10.3390/min11040401 | Journal (article/letter/editorial) | | Article Origin of the Moroccan Touissit-Bou Beker and Jbel Bou Dahar Supergene Non-Sulfide Biomineralization...et al. Origin of the Moroccan Touissit-Bou Beker and Jbel Bou Dahar Supergene Non-Sulfide Biomineralization...Sciences, University Mohammed I, Oujda 60000, Morocco; wissale.boukirou@gmail.com (W.B.); zaid.khdra@gmail...geochemistry, the world-class Touissit- Bou Beker and Jbel Bou Dahar Mississippi Valleytype districts...mineable “calamine” ores in the Touissit-Bou Beker and Jbel Bou Dahar districts. Stable isotope compositions |  | Mondillo, Nicola, Accardo, Mariafrancesca, Boni, Maria, Boyce, Adrian, Herrington, Richard, Rumsey, Mike, Wilkinson, Clara (2020) New insights into the genesis of willemite (Zn2SiO4) from zinc nonsulfide deposits, through trace elements and oxygen isotope geochemistry. Ore Geology Reviews, 118. 103307 doi:10.1016/j.oregeorev.2019.103307 | Journal (article/letter/editorial) | | Museum in London. The specimens are from several deposit-types: 27 1. Stratiform hypogene deposits: Franklin...inhomogeneous, both at the district and at the deposit scale: high-T willemite from the 43 Lusaka area...deposits (Hitzman et al., 2003). In the latter deposit type, 75 willemite locally replaces the original...Schneider et al., 2008; Mondillo et al., 2018), and Morocco (Choulet 97 et al., 2017). 4 98 Until now...Mexico, Saini-Eidukat et al., 2009, 2016; Bou 100 Arhous, Morocco, Choulet et al., 2017; Kabwe, Zambia, |  | | Journal (article/letter/editorial) | | Editor: Nigel Cook] ABSTR ACT The Kabwe Zn-Pb deposit (central Zambia) consists of a cluster of mixed...‘non-sulfide’ is used to define a type of Zn-Pb ore deposit dominated by ‘oxidized’ Zn and Pb ore minerals...sulfides (Hitzman et al., 2003). The Kabwe Zn-Pb deposit (formerly known as ‘Broken Hill’) is located in...Regional geology S90 The rocks underlying the Kabwe region are dominated by Neoproterozoic metasediments which...three main massive sulfide orebodies in the Kabwe region referred to as No. 1, No. 3/4 and No. 5/6, all |
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