The Benue Trough of Nigeria is a polymetallic basin formed from rifting of the central West African basement. The Middle Benue Keana sandstone of Late Cenomanian age is a copper bearing strata within the Keana formation. Mineralization is primarily hosted in gray sandstone capped by a later staged ferruginized band.
Element considerable enriched in the copper bearing sandstone are Mo,Cu and Pb through which copper bearing and non-bearing sandstones can be differentiated with concentration level for this elements reducing from ore bearing strata to ferruginized band to barren reddish/gray sandstone.
Preliminary REE data shows LREE enrichment in the copper bearing sandstones with HREE slightly enriched at the extremities bordering the wall rock.
We hope this data forms a baseline for further exploration to establish areal extent of the mineralization within the basin
![[Visit Client Website]](images/banner.png)