2016
DOI: 10.1016/j.oregeorev.2015.10.011
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The Kalana vein-hosted gold deposit, southern Mali

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Cited by 12 publications
(6 citation statements)
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“…Figure 18 compares the 2D mineralization model for Douta with that for Massawa. These At the WAC scale, similar features appear in a certain number of deposits [31], notably in the Kalana metasediments [24] [65] [66], the Loulo [20] [27]…”
Section: Discussionmentioning
confidence: 90%
“…Figure 18 compares the 2D mineralization model for Douta with that for Massawa. These At the WAC scale, similar features appear in a certain number of deposits [31], notably in the Kalana metasediments [24] [65] [66], the Loulo [20] [27]…”
Section: Discussionmentioning
confidence: 90%
“…These relatively minor, smalldisplacement and/or low-strain deformation events appear restricted to small parts of the Baoulé-Mossi Domain, and likely cannot be correlated across the whole region. Orogenic gold deposits that formed during this period may include the later mineralising event at the Obuasi deposit (Fougerouse et al 2017;Oliver et al 2020), gold mineralisation at the major Ahafo deposit in western-most Ghana (Baah-Danso 2011; Masurel et al 2021), the Siguiri deposit in Guinea (Lebrun et al 2017), and both mineralising events at the Kalana deposit in southern Mali (Salvi et al 2016c).…”
Section: Late Eburnean Gold Deposits (Ca 2095-2060 Ma)mentioning
confidence: 99%
“…According to [73], there are two groups of quartz veins crosscutting a bedding-parallel schistosity surface, striking N170 and dipping steeply towards the E: 1) a first set of groups which show more irregular measured strikes, roughly N-S but some of them are oriented NE-SW and others E-W; 2) a second set of groups, more homogeneous than the other, with closely spaced veinlets striking NE-SW. Both are coeval according to the authors, a point of view shared by Kusters [76] and [78].…”
Section: The Ductile-brittle Deformationmentioning
confidence: 99%