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NIOBIUM-ZIRCONIUM-THORIUM-URANIUM AND RARE-EARTH MINERALS FROM THE PEGMATITES OF SOUTH HARRIS, OUTER HEBRIDES

Journal Article · · Nature
DOI:https://doi.org/10.1038/183255b0· OSTI ID:4260004
Information is presented on mineral occurrences in the Chiapaval and Roneval pegmatites of South Harris, Scotland. The Chiapaval pegmatite vein consists of microcline, albite, and quartz, with a subordinate amount of muscovite as the major mica constituent. Of the minor minerals. topaz, beryl, block-tourmaline, and garnet have been found; the latter mineral seems to be quite abundant locally and was found to contain some 20 per cent of manganese monoxide. In addition, the following minerals have been found: columbite; thorite; uraninite; kasolite; a mineral with an x-ray diffraction pattern almost identical with kasolite, but predominantly a thorium--lead silicate; betafite; zircon; monazite; allanite; and gahnite. The Sletteval pegmatite quarries, east of Roneval, were examined; but apart from apatite no unusual minerals were observed. A pegmatite northeast of Sletteval contained numerous magnetite aggregates which were found to be quite radioactive. Laboratory investigation showed that this pegmatite contained uraninite, thorite, monazite, uranophane, and epidote, together with metamict zircon and allanite, and minor spessartine and pyrites. (J.H.M.)
Research Organization:
The University, Leeds, Eng.
Sponsoring Organization:
USDOE
NSA Number:
NSA-13-007636
OSTI ID:
4260004
Journal Information:
Nature, Journal Name: Nature Vol. Vol: 183
Country of Publication:
Country unknown/Code not available
Language:
English