Channels
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Channels

Channel iron deposits are typically partly eroded and currently are from between 5 km. Mineralised channels are up to 150 kilometres in length, but not all of the preserved length of the CID is of ore grade. Channel iron systems typically form within a depression on the Cenozoic ‘Hamersley Surface’, and form several pods downstream on the palaeodrainage. The channels show typical fluvial sedimentary morphology, with channel scours truncating or incising the channel iron deposits, and rare examples of graded bedding, and so on. Individual ore deposits are subsets of a larger sub-economic mineralized system, which varies laterally and along the palaeodrainage. The deposits form lensoidal accumulations with interbeds of clays, gravels and siliceous detrital materials.

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Company : Jahan Foulad Gharb Complex
Phone : 00982122841596
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Channels

Channel iron deposits are typically partly eroded and currently are from between 5 km. Mineralised channels are up to 150 kilometres in length, but not all of the preserved length of the CID is of ore grade. Channel iron systems typically form within a depression on the Cenozoic ‘Hamersley Surface’, and form several pods downstream on the palaeodrainage. The channels show typical fluvial sedimentary morphology, with channel scours truncating or incising the channel iron deposits, and rare examples of graded bedding, and so on. Individual ore deposits are subsets of a larger sub-economic mineralized system, which varies laterally and along the palaeodrainage. The deposits form lensoidal accumulations with interbeds of clays, gravels and siliceous detrital materials.

Saler Company Information

Company : Jahan Foulad Gharb Complex
Phone : 00982122841596
More Information : View
Online order registration form