Abstract
The southern part of the Bundelkhand craton
contains a series of a E-W trending mafic and ultramafic
rocks, about 40 km in length and 2–4 km wide, that occur
as intrusions within the Bundelkhand Gneissic Complex
(BnGC). They are confined between the Madawara-
Karitoran and Sonrai-Girar shear zones. Dunite, harzburgite,
lherzolite and websterite are the commonly occurring
ultramafic rocks that have high MgO, Ni, Cr, PGE and
low Al2O3, CaO, K2O, TiO2 and V contents, and shows
peridotitic affinity. A distinct trend of crystallization from
peridotite to komatiitic basalt has been inferred from geochemical
plots, which also indicates the occurrence of
at least two varieties among the ultramafic suite of the
Madawara ultramafic complex, namely, Group I comprising
dunite, spinel peridotite, harzburgite and lherzolite,
and Group II consisting of pyroxenite, websterite and
olivine websterite. In several places, the rocks of Group II
have an intrusive relationship with Group I, and are relatively
enriched in total platinum group elements (PGE ~
300 ppb). The discrimination diagrams suggest that the
PGE are enriched in low sulphur-fugacity source magma at
moderate to deeper depths by high degree of partial melting
of the mantle.