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Biotite and amphibole containing up to 4.6 and 5.1 wt% Cl, respectively, are found in gneisses from Black Rock Forest, located within the Hudson Highlands of New York. The area was metamorphosed to granulite facies during the Grenvillian orogeny at ∼ 1100 Ma. Small, subeconomic magnetite deposits coexist with the gneisses.

Cl-rich biotite and amphibole from Black Rock Forest, Cornwall, New York