REE and HFSE mineralization in peralkaline granites of the Ambohimirahavavy alkaline complex, Ampasindava peninsula, Madagascar
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文摘

Rare metals are hosted in granitic dykes emplaced in the rims of the complex.

Granites are ferroan and have a peralkaline affinity.

Mineralization is agpaitic and miaskitic magmatic, and hydrothermal.

The hydrothermal mineralization consists of pseudomorphs after primary minerals.

These granites represent one of very few known occurrence of eudialyte in granite.

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