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The relative mobility of U, Th and Ra isotopes in the weathered zones of the Eye-Dashwa Lakes granite pluton, northwestern Ontario, Canada

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
 [1];  [2]
  1. Geological Survey of Canada, Ottawa, Ontario (Canada)
  2. McMaster Univ., Hamilton, Ontario (Canada)
Radioisotope activity ratios of weathered surface rocks from the Eye-Dashwa Lakes granite pluton show that, in the {sup 238}U decay series, {sup 226}Ra has been leached more rapidly than the grandparent {sup 234}U and {sup 238}U isotopes. The observation of {sup 238}Th/{sup 232}Th disequilibria in the {sup 232}Th decay series shows that either {sup 228}Th (half-life of 1.9 yrs) or {sup 228}Ra (half-life of 5.75 yrs) have been removed from these rocks very rapidly indeed. Isotope ratios of separated mineral fractions appear to show that whereas uranium tends to be removed from all mineral fractions, Ra is strongly readsorbed onto feldspars, presumably as these undergo alteration to clay minerals. This necessitates making a distinction between intermineral mobility of U or Ra, and the net loss of U or Ra from the whole rock. An attempt has been made to model, quantitatively, the transport rate of Ra, though with little success. Failure of the modelling appears to indicate that the mobility of {sup 228}Ra is higher than might be predicted by the mobility of {sup 226}Ra; that is, the two isotopes are not strict analogues of one another in their response to initial weathering.
OSTI ID:
7255877
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 51:10; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English