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After the majority of the silicates dissolve, the aqueous solutions remain. The first chrome ore minerals that have been separated from the melt are brought to the ore deposits in various forms. The difference between these types of beds is that the mineral bed crystallizes before or after the side stone. On the other hand, it is important that the crystallization of the mineral bed occurs in a stagnant and mobile melt, and in various ways, the beds have to be found. If the ore minerals are first separated, they are deposited at the bottom of the magma mass, precipitating in a still solution.

Dudolp Mine