Formation of massive iron deposits linked to explosive volcanic
Magnetite in the outcropping body is coarse-grained (Magnetite-S, >500 µm size) and shows a high degree of alteration to hematite and goethite (Fig. 2a). Iron phosphates and inclusions of monazite and thorium silicate occur in magnetite from the upper levels, particularly at grain rims, or filling both fractures and vesicles.Web
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