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Uranium mineralization in southern
Victoria Land, Antarctica
Incrustations of secondary yellow uranium minerals were found in the radioactive vein locality at the head of the Pyramid Trough. In addition, strongly fluorescent coatings of carbonates containing uranium, were distributed along fractures extending inward at
least 40 centimetres from outcrop surfaces. They furnish clear evidence of mobilization of uranium in solution in the surface-weathering zone. Our preliminary studies indicate that some of the minerals present may be new and previously unknown forms but many show the typical yellowish green fluoresce
that characterizes uranium-bearing carbonate sand phosphates.