Banded Iron Formations (BIF) is the economically prominent litho-units of the Sandur Schist Belt,... more Banded Iron Formations (BIF) is the economically prominent litho-units of the Sandur Schist Belt, hosting high-grade iron ore deposits. Different cycles of formation of these BIF are well-known. In the Joga area, oxide-, carbonate-and sulphide-facies of BIF are recognised. These BIF are more siliceous in nature and belong predominantly to oxide-facies, with clusters of sulphide-facies occurring in tectonically deformed zones. Gold content of the vein quartz associated with BIF of Joga area varies from 0.02 to 0.49 gram per ton.
Banded Iron Formations (BIF) is the economically prominent litho-units of the Sandur Schist Belt,... more Banded Iron Formations (BIF) is the economically prominent litho-units of the Sandur Schist Belt, hosting high-grade iron ore deposits. Different cycles of formation of these BIF are well-known. In the Joga area, oxide-, carbonate-and sulphide-facies of BIF are recognised. These BIF are more siliceous in nature and belong predominantly to oxide-facies, with clusters of sulphide-facies occurring in tectonically deformed zones. Gold content of the vein quartz associated with BIF of Joga area varies from 0.02 to 0.49 gram per ton.
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