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L. Microscopiquement and . Échantillons, Figure IV -4a) xénomorphes, de type orthose (macle Carlsbad), plagioclase et microcline. Les cristaux d'albite automorphes cristallisent sur le pourtour des minéraux de feldspath xénomorphes ou dans les cavités La biotite chloritisée (Figure IV -4b), est présente sous la forme de sections allongées sub-automorphes à xénomorphes de taille inférieure à 1 mm. Les minéraux accessoires sont représentés par le zircon, l'apatite, l'ilménite, la pyrite, l'hématite, l'oxyde de Ti (Figure IV -4d), la magnétite (altérée et affectée localement par des fractures remplies par de la chlorite néoformée (Figure IV -4c)) et des minéraux d'uranium (coffinite) La chlorite est sous forme de minéraux néoformés fibro-radiés, Espinharas sont principalement composés de feldspaths (jusqu'à 50% La calcite et le quartz xénomorphes cristallisent dans les cavités (Figure IV -4e)

. Les-minéraux-d, uranium cristallisent soit : -dans les cavités (Figure IV -5a et b), -autour des magnétites altérées (Figure IV -5b), -en association avec des cristaux de chlorite mais aussi d'ilménite dans les cavités (Figure IV -5c et d)

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