CHARACTERIZATION OF BANDED FERRUGINOUS CHERT AND BANDED IRON FORMATION AND THEIR PROCESSES OF SEDIMENTATION IN THE FIG TREE GROUP, BARBERTON GREENSTONE BELT, SOUTH AFRICA
The lithologic components of BFC and BIF are hematite, siderite, jasper, and pure chert. Petrography and geochemical analyses of our samples show that some bands have more mixed mineralogy than expected. For example, hematite bands contain siderite laminations, and siderite bands have more hematite and mica than siderite. In addition, each band type has a distinct population of rare earth elements (REE). Interestingly, jasper and hematite both have positive Eu anomalies, while siderite does not exhibit a strong Eu anomaly.
The siderite bands exhibit different characteristics from the jasper and hematite bands. The high mica levels, lack of Eu anomaly, and local examples of cross-bedding suggest that the siderite grains were deposited by a combination of currents bringing detrital material and chemical precipitation. These observations are not mirrored in the jasper and hematite bands which have low mica levels, positive Eu anomalies, and planar laminations when present, suggesting exclusively chemical precipitation. We conclude that the BFC was likely deposited at shallower depths than BIF.