2011
DOI: 10.1016/j.jafrearsci.2010.08.001
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Geochronology of the Birim Supergroup of the West African craton in the Wa-Bolé region of west-central Ghana: Implications for the stratigraphic framework

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Cited by 90 publications
(58 citation statements)
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“…This study shows that the Kibi-Asamankese area does not differ significantly from the other Birimian domains of the Leo Rise, with respect to the nature and age of emplacement of the granitoids (e.g., Abouchami et al, 1990;Taylor et al, 1992;de Kock et al, 2011;Sakyi et al, 2014). Three generations of granitoids can be recognised in the study area: the first generation is the Boynton (1984).…”
Section: Implications For Birimian Granitoids In Ghanamentioning
confidence: 67%
“…This study shows that the Kibi-Asamankese area does not differ significantly from the other Birimian domains of the Leo Rise, with respect to the nature and age of emplacement of the granitoids (e.g., Abouchami et al, 1990;Taylor et al, 1992;de Kock et al, 2011;Sakyi et al, 2014). Three generations of granitoids can be recognised in the study area: the first generation is the Boynton (1984).…”
Section: Implications For Birimian Granitoids In Ghanamentioning
confidence: 67%
“…This period is divided into two phases. Though there is regional variation, broadly the Eoeburnean (also known as Eburnean I or the Tangaean; 2266-2150 Ma) precedes the Eburnean (2216-1980 (Taylor et al, 1992;Dia et al, 1997;Loh et al, 1999;Allibone et al, 2002;Gueye et al, 2007;Tshibubudze et al, 2009;Hein, 2010;de Kock et al, 2011). The Eoeburnean consists of volcanism, granitoid emplacement and fold, thrust tectonics, and is interpreted by Tshibubudze et al, (2015) to be a single diachronous event across the Birimian.…”
Section: Geological Settingmentioning
confidence: 99%
“…The geochemistry and isotopic ages of selected samples of batholiths, plutons, dykes and sills related to crystallisation, metamorphism, mineralisation and deformation periods have been published for the WAC by Hirdes et al (1987Hirdes et al ( , 1992Hirdes et al ( , 1996, Lemoine (1988), Milési et al (1989), Leube et al (1990), Liégeois et al (1991), Léger et al (1992), Davis et al (1994), Delor et al (1995aDelor et al ( , 1995b, Pons et al (1995), Ama-Salah et al (1996), Bossière et al (1996), Kouamelan (1996), Abdou et al (1998), Bonnot et al (1998), Daouda-Yao (1998), Doumbia et al (1998), Davis (1998, 2002), Oberthür et al (1998), Potrel et al (1998), Adou (2000), Egal et al (2002), Castaing et al (2003), Gasquet et al (2003), Dioh et al (2006), Feybesse et al (2006), de Kock et al (2011de Kock et al ( , 2012 and Tapsoba et al (2013aTapsoba et al ( , 2013b; in contrast, http://dx.doi.org/10.1016/j.jafrearsci.2015.04.008 1464-343X/Ó 2015 Elsevier Ltd. All rights reserved. only few geochronological ages have been reported for the Oudalan-Gorouol belt (OGB) and the Gorom-Gorom granitoid terrane (GGGT), including the 3 oldest known U-Pb crystallization ages for the West African craton .…”
Section: Introductionmentioning
confidence: 99%