Linked from

The 10 pages that link to Supergene enrichment, each with the reason it gives.

• Porphyry copper depositRelated: Oxidation can move copper downward and create a richer secondary ore blanket.

• Ore depositRelated: Oxidation and downward-moving water can upgrade a deposit after its initial formation.

• AzuriteRelated: The same weathering environment that forms azurite can redistribute copper within deposits.

• Oxidation zoneRelated: Metals leached from the oxidation zone may accumulate below it.

• Native copperRelated: Near-surface alteration can redistribute copper and contribute to native copper formation.

• SmithsoniteRelated: Smithsonite can form as weathering mobilizes zinc from primary ores and redeposits it.

• ErythriteRelated: The same near-surface circulation that enriches ores can precipitate secondary cobalt minerals.

• GreenockiteRelated: Near-surface alteration of zinc ores can redistribute cadmium into greenockite.

• HemimorphiteRelated: Oxidizing groundwater transports zinc that can contribute to hemimorphite formation.

• Arsenate mineralRelated: Groundwater moves metals and arsenic through the zones where secondary arsenates form.