1	-	Jacquemin, H., Sheppard, S. M., & Vidal, P. (1982). Isotopic geochemistry (O, Sr, Pb) of the Golda Zuelva and Mboutou anorogenic complexes, North Cameroun: mantle origin with evidence for crustal contamination. Earth and Planetary Science Letters, 61(1), 97-111. doi.org/10.1016/0012-821X(82)90042-5

Confirmation

Validity:

Believed Valid

Data

Mineral Data:

Click here to view Granite data

Locality Data:

Click here to view Golda Zuelva Complex, Far North Region, Cameroon

Data Identifiers

Mindat Occurrence Record ID:

1421929

Long-form Identifier:

1:3:1421929:8

GUID (UUID V4):

Nearest other occurrences of Granite

31.7km (19.7 miles)

ⓘ Grea Intrusion, Far North Region, Cameroon

References

Lasserre, M. (1966). Confirmation de l'existence d'une série de granites tertiaires au Cameroun (Afrique équatoriale). Bulletin du Bureau de recherches géologiques et minières, (3), 141-148.

Lasserre, M. (1978). MISE AU POINT SUR LES GRANITOIDES DITS" ULTIMES" DU CAMEROUN: GISEMENT, PETROGRAPHIE ET GEOCHRONOLOGIE. Bulletin du Bureau de Recherches Geologiques et Minieres, Paris, 4, 143-159.

Jacquemin, H., Sheppard, S. M., & Vidal, P. (1982). Isotopic geochemistry (O, Sr, Pb) of the Golda Zuelva and Mboutou anorogenic complexes, North Cameroun: mantle origin with evidence for crustal contamination. Earth and Planetary Science Letters, 61(1), 97-111. doi.org/10.1016/0012-821X(82)90042-5

Déruelle, B., Moreau, C., Nkoumbou, C., Kambou, R., Lissom, J., Njonfang, E., Ghogomu, R. T., Nono, A. (1991) The Cameroon Line: A Review. In Magmatism in Extensional Structural Settings. Springer Berlin Heidelberg. p.274-327. doi:10.1007/978-3-642-73966-8_12

Reference Search (possible matching items)

👁 Image	Jacquemin, Hervé, Sheppard, Simon M.F., Vidal, Philippe (1982) Isotopic geochemistry (O, Sr, Pb) of the Golda Zuelva and Mboutou anorogenic complexes, North Cameroun: mantle origin with evidence for crustal contamination. Earth and Planetary Science Letters, 61 (1) 97-111 doi:10.1016/0012-821x(82)90042-5	Journal (article/letter/editorial)
	geochemistry (0, Sr, Pb) of the Golda Zuelva and Mboutou anorogenic complexes, North Cameroun" mantle origin...annular (6-8 km diameter) Golda Zuelva and Mboutou anorogenic complexes of North Cameroun are composed of...olivine gabbro to amphibole and biotite granite. For the Mboutou complex there are two overlapping centres...centres. In the Golda Zuelva complex the plutonic rocks are associated with a later hawaiite to rhyolite volcanic...isochron gives an age of 6 6 = 3 Ma for the Golda Zuelva granites, with initial 87Sr/86Sr ratio of 0

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⇱ Granite from Golda Zuelva Complex, Far North Region, Cameroon

Granite from
Golda Zuelva Complex, Far North Region, Cameroon