"The quantitative study of the supergene evolution of ultramafic rocks was especially carried out in the great peridotitic massive of Southern New Caledonia. The scheme of this work is the following: geomorphological study of the landscape, mineralogical and geochemical study of the residual phase in the weathering profiles, chemical study of the soluble phase in waters, and valuation of the geochemical balance of weathering, erosion and transportation processes. About twenty weathering profiles and 700 samples of spring water, ground waters and river waters were analysed."
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