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Pearce, J. (1996) A User’s Guide to Basalt Discrimination Diagrams. In: Wyman, D.A., Ed., Trace Element Geochemistry of Volcanic Rocks: Applications for Massive Sulfide Exploration, Geological Association of Canada, St. John’s, Short Course Notes, Vol. 12, 79-113.

has been cited by the following article:

• TITLE: Petrology and Structural Characterization of Post-Neoproterozoic Dolerites from the Kimberlite Fields in the Kéniéba Region (Western Mali)

  AUTHORS: Gbele Ouattara, Baco Traore, Ziandjêdé Hervé Siagné, Aboubacar Denon, Souleymane Sangare, Marc Ephrem Allialy

  KEYWORDS: Dolerites, Kimberlitic Fields, Petrology, Structures, Kéniéba, Mali

  JOURNAL NAME: Open Journal of Geology, Vol.14 No.6, June 18, 2024

  ABSTRACT: Post-Neoproterozoic dolerites from the Kéniéba region (Western Mali) are often associated with kimberlites. The rarity of kimberlite outcrops led to the study of doleritic rocks, spatially associated with them. The petrographic and lithogeochemical study showed that the dolerites of the Kéniéba kimberlitic fields are of tholeiitic nature and of the E-MORB (Enriched-Mid Ocean Ridge Basalt) type. This reflects an enrichment over time, compared to the Birimian dolerites of the volcano-sedimentary greenstone belt of Toumodi, in central C?te d’Ivoire. Furthermore, these dolerites are enriched in SiO2, TiO2, Zr and poor in Fe2O3, MgO. These dolerites would have formed in a late to post-orogenic intracontinental context during the breakup of Gondwana. Structurally, Kéniéba dolerites are often associated with kimberlite pipes, fractures and large deep structures identified using aeromagnetic images. Taking into account the fact that kimberlites do not outcrop in the Kéniéba region, the geochemical study coupled with the interpretation of aeromagnetic data proved to be very useful for the search for pipes.