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Baratoux, L., Söderlund, U., Ernst, R.E., de Roever, E., Jessell, M.W., Kamo, S., et al. (2018) New U-Pb Baddeleyite Ages of Mafic Dyke Swarms of the West African and Amazonian Cratons: Implication for Their Configuration in Supercontinents through Time. In: Srivastava, R., Ernst, R. and Peng, P., Eds., Dyke Swarms of the World: A Modern Perspective, Springer, 263-314.
https://doi.org/10.1007/978-981-13-1666-1_7

has been cited by the following article:

• TITLE: Hydrothermal Alteration Associated with the Kiaka World-Class Gold Deposit (Burkina Faso, West Africa)

  AUTHORS: Benjamin Sawadogo, Gounwendmanaghré Hubert Zongo, Wilédio Marc-Emile Bonzi, Kalidou Traore, Sâga Sawadogo, Ousseni Yameogo, Ousmane Bamba, Guy Franceschi

  KEYWORDS: Gold Deposit, Hydrothermal Alteration, Deformation, Geochemistry, Burkina Faso

  JOURNAL NAME: Open Journal of Geology, Vol.14 No.12, December 6, 2024

  ABSTRACT: This paper aims to show the relationships between hydrothermal alteration, deformation and gold mineralization in the main area of the Kiaka deposit. The Kiaka gold deposit is located in the South-central of Burkina Faso in the Tenkodogo volcano-sedimentary belt. Mineralization is primarily hosted by amphibolite, mylonitized quartz microdiorite and meta-sediment. The combination of petrographic, metallographic and geochemical analysis along with structural deformation of the ore body allowed us to distinguish the three main stages of hydrothermal alteration in the Kiaka gold deposit. (i) The first stage is characterized by ductile deformation which induces potassic- and LILE-rich alteration with crystallization of disseminated pyrrhotite. (ii) The second stage corresponds to chloritization and is associated with a brittle-ductile deformation and retrograde metamorphism. A second generation of disseminated pyrrhotite and a few pyrite and chalcopyrite crystallized during this event. Pyrrhotite also fills veins. (iii) The third alteration stage is characterized by a significant carbonation and concurrent with a brittle deformation. It is accompanied locally by a high-grade gold mineralization (up to 29 g/t).