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Working Iron and Copper Deposits by Open Pits

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Abstract

Four minerals are the main source of the iron of commerce. They are magnetite, Fe3O4, with a theoretical iron content of 72% and sometimes known as ‘black’ or ‘magnetic ore’; haematite, Fe2O3, is a red ore with 70% iron; limonite, 2Fe2O33H2O, is a yellowish-brown ore with varying amounts of water in its composition and contains 60% iron; siderite, FeCO3, known also as chalybite or spathic iron ore has a theoretical iron content of 48%. In addition other important iron deposits such as those worked in the Midlands and in France are partly composed of greenish hydrous iron silicates such as chamosite and greenalite with siderite.

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References

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© 1969 Elsevier Publishing Company Limited

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Sinclair, J. (1969). Working Iron and Copper Deposits by Open Pits. In: Quarrying Opencast and Alluvial Mining. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-7611-8_7

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  • DOI: https://doi.org/10.1007/978-94-011-7611-8_7

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-011-7613-2

  • Online ISBN: 978-94-011-7611-8

  • eBook Packages: Springer Book Archive

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