2021
DOI: 10.1080/00206814.2021.1998799
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Cryogenian crustal evolution in western Nigeria shield: whole-rock geochemistry, Sr-Nd and zircon U-Pb-Hf isotopic evidence from Bakoshi-Gadanya granites

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Cited by 11 publications
(2 citation statements)
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“…After a prolonged period of quiescence, the Nigeria basement was intruded by Neoproterozoic granites (825–500 Ma; “Older granites”) during collision and welding of the West African Craton with Congo and East Saharan cratonic blocks along the Trans‐Saharan Belt (Ferré et al., 2002; Ominigbo, 2022; Toteu et al., 2004). In the North Nigeria basement, granites were mainly intruded between 710 and 500 Ma (Elatikpo et al., 2022 and references therein) but Tonian (825–764 Ma) intrusive rocks also occur locally (Goodenough et al., 2014; Ogezi, 1977). Granitoid intrusions of similar ages occur in the SW Nigeria basement (715–580 Ma; Ferré et al., 1996; Tubosun et al., 1984).…”
Section: The Niger Rivermentioning
confidence: 99%
“…After a prolonged period of quiescence, the Nigeria basement was intruded by Neoproterozoic granites (825–500 Ma; “Older granites”) during collision and welding of the West African Craton with Congo and East Saharan cratonic blocks along the Trans‐Saharan Belt (Ferré et al., 2002; Ominigbo, 2022; Toteu et al., 2004). In the North Nigeria basement, granites were mainly intruded between 710 and 500 Ma (Elatikpo et al., 2022 and references therein) but Tonian (825–764 Ma) intrusive rocks also occur locally (Goodenough et al., 2014; Ogezi, 1977). Granitoid intrusions of similar ages occur in the SW Nigeria basement (715–580 Ma; Ferré et al., 1996; Tubosun et al., 1984).…”
Section: The Niger Rivermentioning
confidence: 99%
“…Most gold occurrences in the Paleoproterozoic grounds of the West African Craton are orogenic gold deposits formed during the Eburnian cycle about two billion years ago [ [1] , [2] , [3] , [4] ]. The formation of these deposits is directly related to crustal accretion or collisional processes in a subduction context and can be developed in arc, back-arc or accretionary prism environments [ 5 ].…”
Section: Introductionmentioning
confidence: 99%