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Map of permissive tract sedfe01—Haji Gak Neoproterozoic for undiscovered sedimentary ýrock-hosted iron deposits, showing distribution of Neoproterozoic rocks that host the Haji ýGak iron deposit
Hajigak deposit
The best known iron-oxide deposit in Afghanistan is located about 100 km west of Kabul ýin Bamyan Province, although mineralisation of this style has been identified ýdiscontinuously in an east-west belt over 600 km from Herat to the Panjsher River. The ýiron-bearing formations are in a sequence of sedimentary and volcanic rocks
of Proterozoic age.ý
The deposit extends over 32 km and contains 16 separate zones, up to 5 km in length, 380 ým wide and extending 550 m down dip, seven of which have been studied in detail. The ýore occurs in both primary and oxidised states.

The primary ore (80% of the deposit) ýoccurs below 100-130 m and comprises magnetite and ýpyrite, with minor other sulphides ýincluding chalcopyrite, and averages 61.3% Fe, 5% sulphide ýand 0.05% P. The remaining ýý20% is oxidised and consists of three hematitic ore types at ýý62.8% Fe. The mineralisation ýis believed to be partly structurally controlled and related to ýOligocene magmatism. ýRussian estimates for the entire deposit are 1 700 Mt, although ýestimates for the near ýsurface oxide ore in the most explored area are 85 Mt (Category A-C2). ýA feasibility ýstudy on the deposit was undertaken in 1972 by a Franco-German group and ýincluded the ýconstruction of a blast furnace.ý |