The rare earth element (REE) mineralization of Gakara (Burundi) has first been discovered in 1936 and has periodically been the subject of geological studies, at times when the exploitation of bastnäsite-(Ce) and monazite-(Ce) was economically interesting.
This study focuses on the establishment of a mineral paragenesis for Gakara, with special attention to the REE-bearing phases, to understand the formation history of the deposit.
The paragenesis can be subdivided into 3 stages: primary ore deposition, brecciation stage and supergene alteration. Evidence for fenitization processes (i.e. pinkish-red cathodoluminescence of K-feldpar, brecciation stage) and the strong enrichment of light REEs in bastnäsite and monazite substantiate the hypothesis of a structurally controlled hydrothermal mineralization with a strong carbonatitic affinity.
Rainbow Rare Earths Ltd (LON:RBW) is a mining company focussed on production from, and expansion of, the high grade Gakara Rare Earth Project in Burundi, East Africa. With in-situ grades in the range of 47-67% Total Rare Earth Oxide (TREO), Gakara is one of the world’s richest rare earth deposits.