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URANIUM MINERALIZATION IN ROCKS OF THE BERNHARD CYRSTALLINE LAYER (in German)

Journal Article · · Experientia (Switzerland)
OSTI ID:4304016
Radioactive rocks were round in the layers of the Grande Dixence S.A. X- ray, chemical, and chalcographic analyses have shown the presence of uranium in the form of pitchblende. The mineralization is shown, in the sandstone and chlonitic mica schists, by dark horizons. The pitchblende is associated with pyrite, chalcopyrite, galena, covellite, and hematite. At another . location mineralization is not apparent. The radioactive rock is a carbonate sericitic quartz containing uranium. (tr-auth)
Research Organization:
Originating Research Org. not identified
NSA Number:
NSA-12-015559
OSTI ID:
4304016
Journal Information:
Experientia (Switzerland), Journal Name: Experientia (Switzerland) Vol. Vol: 14; ISSN EXPEA
Country of Publication:
Country unknown/Code not available
Language:
German

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