Work carried out to date indicates that the Maracás vanadium-rich titaniferous magnetite deposit is situated in a geologic environment similar to other magmatic vanadium-rich magnetite deposits. The Rio Jacaré intrusion that hosts the deposit is a mafic to ultramafic layered intrusion characterized by both rhythmic and cryptic layering that includes a pyroxenite/gabbro layer in the upper part. This gabbro layer hosts the Campbell vanadium deposit. The deposit has been assigned this way by the manner in which it was generated as an early magmatic ore type deposit formed by concentration through liquid immiscibility.

The primary minerals of the gabbro layer are plagioclase, augite and magnetite. Secondary alteration has altered most of the augite to uralite. Plagioclase occurs as elongated laths, the only idiomorphic mineral present, with the allotriomorphic minerals of magnetite and augite occurring as grains between the plagioclase laths. Magnetite was the last mineral to crystallize and, because of the amount of vanadium incorporated in it, the magnetite gabbro layer has the potential to have economic value. The crystal form of the magnetite does not indicate the concentration of the magnetite by an accumulation of separate magnetite crystals; on the contrary, the textural features suggest the formation of a separate oxide liquid.

The enrichment of PGMs, in association with magnetite, has been described in other mafic ultramafic complexes. In association with the Main Magnetite Layer in the Upper zone of the Bushveld Complex, PGMs are concentrated in anorthosite just below the layer. However, the magnetite seams themselves contain very little PGMs.

In the Skaergaard intrusion in Greenland, palladium is concentrated with copper and gold in anorthositic layers associated with magnetite at the top of the middle zone, having values of up to 3 ppm Pd and 200 ppb Pt. In the Rincón del Tigre Complex in Bolivia, platinum and palladium are concentrated with copper at the base of the magnetite-bearing gabbro in the upper part of the intrusion with maximum precious metals concentrations of 1.8 ppm Pd and 0.68 ppm Pt in separate 1-m samples. In all of these intrusions, magnetite formed after extensive fractionation of the magma.

The sulphide content of the Rio Jacaré rocks is very low and the rocks are metamorphosed. Sulphides in the magnetite and magnetite bearing pyroxenite of the Lower zone show enrichment in platinum, palladium, rhodium, iridium, gold and nickel, but not in copper, compared to the Upper zone. Recalculated sulphide concentrations for samples from Campbell are similar to those of PGM-enriched sulphides from Birch Lake and Medvezhy Creek in the Norilsk Complex. In contrast, recalculated sulphide concentrations of the Gulçari B and Novo Amparo samples resemble the PGM-depleted Minnimax sulphides and Dunka Road sulphides of the Duluth Complex.

The vanadium at Maracás is associated with the titaniferous magnetite. Within the deposit, the titaniferous magnetite is the major oxide phase, followed by ilmenite. Magnetite occurs as primary grains that may be partly martitized. There is also fine-grained magnetite as inclusions in the silicate grains. This magnetite occurs as a secondary alteration after uralitization of pyroxene and serpentinization of olivine.

The magnetite normally occurs as anhedral grains, with grain sizes of between 0.3 and 2.0 mm, and forms a polygonal mosaic together with ilmenite. Ilmenite also occurs as inclusions in the magnetite, commonly displaying exsolution textures. Silicate phases associated with the magnetite include uralite, augite, plagioclase, hornblende, and rare grains of clinopyroxene, olivine and spinel. Magnetite from the magnetitite in the Lower zone (Campbell) has higher V2O5 concentrations (0.9% to 7.0%) than magnetite from the Upper zone (Gulçari B and Novo Amparo, 0.3% to 2.5% V2O5; Brito, 2000).

Rare olivine and pyroxene grains are observed within the magnetitite, but most are altered to serpentine or chlorite. The Rio Jacaré intrusion has been intensely metamorphosed, so the pyroxene compositions observed probably reflect metamorphic re-equilibration rather than original magmatic compositions. In addition, Brito (2000) also documented the presence of orthopyroxene. Garnet and biotite are present in the Gulçari B and Novo Amparo deposits.

The Maracás Vanadium Project is an open pit operation utilizing a contract mining fleet of hydraulic excavators, front-end loaders and 36 tonne haul trucks.

The disposal of waste rock, and low grade mineralized material will be executed on an area close to the pit. The site shall be adequately prepared to include drainage at its base and channels to direct the flow of water with the aim of aiding geotechnical stability and mitigating the erosion of the stockpiled material.

The operation of this phase, in accordance with the ascending method, shall begin during the construction of the heap at the base of this area. Waste rock will be disposed by truck, which will then be uniformly distributed and leveled by an operator using a tractor. The procedure is then repeated, stacking another bank above the original one, while maintaining a ramp for the trucks to be able to access the area.

The Maracás vanadium recovery plant was commissioned in 2015 and has been in startup mode for much of that time ramping up to near design capacity. At the time of writing this report, the plant produces up to 9,360 t of V2O5 equivalent per year with a trend approaching design capacity. Except for unanticipated downtime and subject to completion of the two expansions contemplated herein, production is expected to reach 13,200 t/a V2O5 in 2020.

The current process flow sheet comprises three stages of crushing, one stage of grinding, two stages of magnetic separation, magnetic concentrate roasting, vanadium leaching, ammonium meta-vanadate (AMV) precipitation, AMV filtration, AMV calcining, and fusing to V2O5 flake as final product.

Originally sized to process 960,000 tpy run of mine (ROM) the plant will be capable, after due modification, to process 1,900,000 tpy of feed ore with an average grade of 1.14% V2O5 and produce 9,600 t/y V2O5.in 2017. In 2020 after comple ........