T
he late Arc
haean volcanic rocks of t
he Iramba–Sekenke greenstone belt consist of t
holeiitic basalts and basaltic andesites t
hat are associated wit
h a subordinate amount of intermediate to felsic volcanic rocks. Sm–Nd geoc
hronology s
hows t
hat t
he entire volcanic suite was emplaced at 2742 ± 27 Ma (MSWD = 1.6,
http://www.sciencedirect.com/scidirimg/entities/25b.gif"" alt=""var epsilon"" title=""var epsilon"" border=""0"">Nd = 2.3).