Figure 5. (g, h) fine grained mesh of epidote, tremolite, talc and actinolite. These minerals are brightly coloured and display plumose and decussate radiating textures controlled by the cleavage planes plagioclase, (i) euhedral cubic crystals of sulphide mineral with etched section. The etched edges have been occupied by chlorite and actinolite altered from the primary silicate minerals

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Mineral Alteration and Chlorite Geothermometry in Platinum Group Element (PGE)- Bearing Meta-ultramafic Rocks from South East Cameroon

Ako T. A., A. Vishiti, K. I. Ateh, A. C. Kedia, C. E. Suh

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