The nature and distribution of carbonate minerals in the upper Qu'Appelle basin in S-central Saskatchewan were investigated. The equivalent carbonate content and calcite:dolomite ratios of the deposits reflect the mechanisms of glacial deposition and some differences in the sources of the original parent material. A good correlation exists between the lake water ionic activity products for CaCO3 and the relative equivalent carbonatic mineral contents of the sediments.-from Authors
CITATION STYLE
Ghebre-Egziabhier, K., & St. Arnaud, R. J. (1983). Carbonate mineralogy of lake sediments and surrounding soils. 2. The Qu’Appelle lakes ( Canada). Canadian Journal of Soil Science, 63(2), 259–269. https://doi.org/10.4141/cjss83-026
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