A. Cheilletz et al., COOLING AGE OF THE BIRIMIAN JUVENILE CRUS T IN WEST-AFRICA - U-PB, RB-SR AND K-AR DATA ON THE 2.1 GA GRANITE-GREENSTONE TERRAINS FROM SW NIGER, Comptes rendus de l'Academie des sciences. Serie II. Mecanique, physique, chimie, astronomie, 319(4), 1994, pp. 435-442
A comparison between zircon U-Pb, whole-rock Rb-Sr and biotite-amphibo
le K-Ar data on Birimian granite-greenstone terrains from SW-Niger ind
icates that the youngest granitic plutons were emplaced at 2,115+/-5 M
a and that both the plutons and the surrounding greenstones yield cool
ing ages around 2,118 Ma. The age similarity between the end of the pl
utonism and the cooling of plutons and surrounding greenstone further
suggests rapid cooling at the end of the plutonic event and, thus, cor
roborates a model of greenstone metamorphism linked to the thermal eff
ect of the plutons.