Geochemistry and geochronology of the ~620 Ma gold-associated Batouri granitoids, Cameroon

The Batouri gold mining area in southeastern Cameroon is part of the Adamawa-Yadé Domain of the Central African Fold Belt (Pan-African). It is underlain by a variety of granitic rocks, including alkali-feldspar granite, syeno-monzogranite, granodiorite, and tonalite. Geochemical data suggest that th...

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Published inInternational geology review Vol. 57; no. 11-12; pp. 1485 - 1509
Main Authors Asaah, Akwinga Victor, Zoheir, Basem, Lehmann, Bernd, Frei, Dirk, Burgess, Ray, Suh, Cheo Emmanuel
Format Journal Article
LanguageEnglish
Published Philadelphia Taylor & Francis 10.09.2015
Taylor & Francis Ltd
Subjects
Batouri granitoids
Cameroon
geochemical characteristics
tectonic evolution
U-Pb and Ar/Ar geochronology
Online AccessGet full text
ISSN0020-6814
1938-2839
DOI10.1080/00206814.2014.951003

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Abstract The Batouri gold mining area in southeastern Cameroon is part of the Adamawa-Yadé Domain of the Central African Fold Belt (Pan-African). It is underlain by a variety of granitic rocks, including alkali-feldspar granite, syeno-monzogranite, granodiorite, and tonalite. Geochemical data suggest that these rocks formed by differentiation of I-type tonalitic magma under oxidizing conditions in a continental volcanic arc setting. U-Pb dating of zircons from gold-associated monzogranite-granodiorite at Kambélé gave concordant ages of 619 ± 2 and 624 ± 2 Ma, while Ar-Ar dating of alkali-feldspar granite yielded a non-plateau maximum age of 640-620 Ma. These ages imply that the Batouri granitoids were emplaced during the collision of the West African Craton and the Congo Craton. The geochemical characteristics of the Batouri granitoids as well as their oxidized state (magnetite series) are typical of gold-associated felsic rocks in subduction settings elsewhere. The similarities in age, composition, and geochemical affinities of these granitoids with those reported from other localities in the Adamawa-Yadé Domain reinforce the earlier assumption that the granitic rocks of this domain represent parts of a regional-scale batholith, with commonly small-scale, high-grade auriferous quartz veins in structurally favourable sites. The spatial and temporal association of gold mineralization and the Batouri granitoids may suggest potential for regional-scale, high-tonnage, granite-related gold ore.
AbstractList The Batouri gold mining area in southeastern Cameroon is part of the Adamawa-Yadé Domain of the Central African Fold Belt (Pan-African). It is underlain by a variety of granitic rocks, including alkali-feldspar granite, syeno-monzogranite, granodiorite, and tonalite. Geochemical data suggest that these rocks formed by differentiation of I-type tonalitic magma under oxidizing conditions in a continental volcanic arc setting. U-Pb dating of zircons from gold-associated monzogranite-granodiorite at Kambélé gave concordant ages of 619 ± 2 and 624 ± 2 Ma, while Ar-Ar dating of alkali-feldspar granite yielded a non-plateau maximum age of 640-620 Ma. These ages imply that the Batouri granitoids were emplaced during the collision of the West African Craton and the Congo Craton. The geochemical characteristics of the Batouri granitoids as well as their oxidized state (magnetite series) are typical of gold-associated felsic rocks in subduction settings elsewhere. The similarities in age, composition, and geochemical affinities of these granitoids with those reported from other localities in the Adamawa-Yadé Domain reinforce the earlier assumption that the granitic rocks of this domain represent parts of a regional-scale batholith, with commonly small-scale, high-grade auriferous quartz veins in structurally favourable sites. The spatial and temporal association of gold mineralization and the Batouri granitoids may suggest potential for regional-scale, high-tonnage, granite-related gold ore.
The Batouri gold mining area in southeastern Cameroon is part of the Adamawa-Yadé Domain of the Central African Fold Belt (Pan-African). It is underlain by a variety of granitic rocks, including alkali-feldspar granite, syeno-monzogranite, granodiorite, and tonalite. Geochemical data suggest that these rocks formed by differentiation of I-type tonalitic magma under oxidizing conditions in a continental volcanic arc setting. U-Pb dating of zircons from gold-associated monzogranite-granodiorite at Kambélé gave concordant ages of 619 ± 2 and 624 ± 2 Ma, while Ar-Ar dating of alkali-feldspar granite yielded a non-plateau maximum age of 640-620 Ma. These ages imply that the Batouri granitoids were emplaced during the collision of the West African Craton and the Congo Craton. The geochemical characteristics of the Batouri granitoids as well as their oxidized state (magnetite series) are typical of gold-associated felsic rocks in subduction settings elsewhere. The similarities in age, composition, and geochemical affinities of these granitoids with those reported from other localities in the Adamawa-Yadé Domain reinforce the earlier assumption that the granitic rocks of this domain represent parts of a regional-scale batholith, with commonly small-scale, high-grade auriferous quartz veins in structurally favourable sites. The spatial and temporal association of gold mineralization and the Batouri granitoids may suggest potential for regional-scale, high-tonnage, granite-related gold ore.
Author Zoheir, Basem
Asaah, Akwinga Victor
Suh, Cheo Emmanuel
Burgess, Ray
Lehmann, Bernd
Frei, Dirk
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Snippet The Batouri gold mining area in southeastern Cameroon is part of the Adamawa-Yadé Domain of the Central African Fold Belt (Pan-African). It is underlain by a...
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SubjectTerms Batouri granitoids
Cameroon
geochemical characteristics
tectonic evolution
U-Pb and Ar/Ar geochronology
Title Geochemistry and geochronology of the ~620 Ma gold-associated Batouri granitoids, Cameroon
URI https://www.tandfonline.com/doi/abs/10.1080/00206814.2014.951003
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Volume 57
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