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The Highest Iron Gold Magnetite Siderite

Chlorite in altered BIF occurs as tabular grains intergrown with, or replacing, magnetite, siderite, quartz, dolomite, and pyrite (Fig. 5e, f). Based on the magnetite–hematite–quartz ( siderite) assemblage, the Amalia BIF is classified as an oxide ( carbonate) facies BIF (after James, 1954). 2.2.3 Interbedded schist

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