secondary mineral
Quick Summary
Secondary minerals are formed after the original solidification of an igneous rock, typically through processes like weathering or hydrothermal alteration. This contrasts with primary minerals, which crystallize during the rock's initial formation. Secondary enrichment is a significant process where valuable ore minerals are dissolved and redeposited, leading to more concentrated deposits. This is particularly important for copper sulfides under desert weathering conditions and can significantly increase the iron content in banded iron formations.12
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