Baratoux Lenka, Metelka V., Naba S., Ouiya P., Siebenaller Luc, Jessell Mark, Nare A., Salvi S., Beziat D., Franceschi G. (2015). Tectonic evolution of the Gaoua region, Burkina Faso : implications for mineralization. In :
Jessell Mark (ed.), Liégeois J.P. (ed.). Tectonics, mineralisation and regolith evolution of the West African Craton. Journal of African Earth Sciences, 112, part B (No spécial), p. 419-439. ISSN 1464-343X.
Titre du document
Tectonic evolution of the Gaoua region, Burkina Faso : implications for mineralization
Année de publication
2015
Auteurs
Baratoux Lenka, Metelka V., Naba S., Ouiya P., Siebenaller Luc, Jessell Mark, Nare A., Salvi S., Beziat D., Franceschi G.
In
Jessell Mark (ed.), Liégeois J.P. (ed.), Tectonics, mineralisation and regolith evolution of the West African Craton
Source
Journal of African Earth Sciences, 2015,
112, part B (No spécial), p. 419-439 ISSN 1464-343X
The interpretation of high-resolution airborne geophysical data integrated with field structural and lithological observations were employed in the creation of a litho-structural framework for the Gaoua region, Burkina Faso. The granite-greenstone domain of Paleoproterozoic age was affected by multiple deformation and mineralization events. The early tectonic phase is characterized by the emplacement of voluminous tholeiitic and calc-alkaline lavas, probably in a volcanic arc setting. The copper mineralization in Gongondy, Dienemera and Mt Biri is concentrated in a diorite/andesite breccia, and is interpreted as porphyry-copper style formed at an early stage of the evolution of the area. Evidence for the first deformation event D1(Ga) corresponding to N-S shortening was only found in the E-W trending mafic unit bordering the Gaoua batholith to the south. A second deformation phase D2(Ga) occurred under greenschist facies conditions and lead to a development of more or less penetrative metamorphic foliation and its subsequent folding under overall E-W compression. At later stages, the D2(Ga) switched to a transcurrent regime characterized by intense N-S to NW-trending steeply dipping shear zones. The first significant gold mineralization event is related to this transcurrent tectonic phase. During subsequent D3(Ga), intense network of brittle to brittle ductile NW and NE faults developed. Economic gold concentrations are attributed to the D3(Ga) event and are associated with the remobilization of early disseminated low grade gold concentrations. Significant deposits in the area are Nassara, Gomblora, Batie West and Kampti. The last deformation event D4(Ga) resulted in E-W trending thrust faults and crenulation cleavage planes, under overall N-S compression. No mineralization events related to this stage have been seen.
Plan de classement
Géologie et formations superficielles [064]
;
Géophysique interne [066]
Description Géographique
BURKINA FASO
Localisation
Fonds IRD [F B010066068]
Identifiant IRD
fdi:010066068
