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Abstract (EN):
Saprolites or “in situ” weathering products from granitoid rocks of Northwest Portugal were studied by means of X-ray diffraction of their clay fraction and observations of polished thin sections combined with TEM, SEM-EDS microanalyses. Their principal features are: (1) depths of more than 10 m; (2) mean material loss of 40% as calculated by an isovolumetric method; (3) low clay content (mean value 7%) and a high degree of mineralogical evolution. The clay fraction is characterized by a predominance of kaolinite and gibbsite, with subordinate 2:1 minerals (illite, chlorite, vermiculitic mixed-layers, vermiculite). The significance of the secondary minerals in granitic saprolites from Northwest Portugal is compared to published data from Atlantic Europe. This allows the definition of a climatic zonality for weathering products and identifies ‘arenization’ as an important weathering process.
Idioma:
Português
Tipo (Avaliação Docente):
Científica
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