HEMATITE AND GOETHITE INCLUSIONS IN LOW-GRADE DOLOMITIC BANDED IRON FORMATIONS: PHYSICAL PARAMETER EVALUATION TO OPTIMIZE ORE BENEFICIATION

Abstract

International audienceBanded iron formations (BIFs) comprise complex textures and mineralogy, which result from fluid-rock interactions related to high and low temperature alteration. The initial iron oxy hydroxide mineralogy and associated phases such as carbonates, quartz, apatite and phyllosilicates were transformed leading to an upgrading of these BIFs into the world's largest source of iron ore. In low-grade BIFs, a large part of the iron is related to micro-and nano-metric iron-bearing inclusions within micrometric quartz and/or carbonates (mainly dolomite). We studied laminated jaspilitic BIF samples from a drill core containing 26.71 wt.% total iron, 0.2 wt.% SiO 2 , 0.32 wt.% MnO, 15.46 wt.% MgO, 22.32 wt.% CaO, 0.09 wt.% P 2 O 5 , < 0.05 wt.% Al 2 O 3 , 0.15 wt.% H 2 O and 34.08 wt.% CO 2 (Àguas Claras Mine, Quadrilátero Ferrífero, Brazil). Bright rose coloured dolomite and quartz bands alternate with massive specular hematite bands. Raman spectroscopy, X-ray diffraction and FIB-TEM analyses reveal that the micro-and nano-metric inclusions in dolomite are mainly hematite and minor goethite, partly occurring as clusters in voids. Curie Balance analyses were carried out at different heating steps and temperatures on whole rock samples and a synthetic mix of decarbonated sample and pure dolomite. X-ray diffraction on the products of the heating experiments shows that that hematite is stable and new phases: magnesioferrite (MgFe 2 O 4), lime (CaO), periclase (MgO), portlandite (Ca(OH) 2) and srebrodoskite (Ca 2 Fe 2 O 5) were formed between 680°C and 920°C. These finding gives hints to optimizing the beneficiation process, as the presence of hydroxyl ions bearing goethite micro-and nanoinclusions lowers the sintering temperature. Prior separation of coarse hematite and barren dolomite and quartz, followed by lower temperature sintering of the inclusion-bearing dolomite/quartz leads to transformations into phases with higher magnetic susceptibilities (such as hematite and magnesioferrite). The entire Fe and Fe/Mg oxide feed (the priorly separated fraction added to the sintered fraction) can then pass through wet-high intensity magnetic separation after crushing