Hydrous Iron Phosphates in the Chondritic Impact Melt Breccia NWA 4218

Physics

Scientific paper

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Scientific paper

The chondritic melt rock NWA 4218 contains within the melt matrix
regions rich in an iron phosphate mineral. The hydrous phosphate could
be formed either (1) by weathering in an acid environment or (2) by
terrestrial alteration of a primary phosphate.

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