LES CARACTÉRISATIONS DES FELDSPATHS DU MASSIF D’OUED EL-ANNAB ET LA POSSIBILITÉ DE LES EXPLOITER POUR L’INDUSTRIE

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Hassni Belaidi
Saida Kitouni
Smaine Chellat

Abstract

Les microgranites du massif d’Oued El-Annab font partie des roches magmatiques calciques riches en K d’âge Miocène, ils sont exposés sur une superficie d’environ 150 km2 dans le cap de fer et Edough sur le long de la côte méditerranéenne nord-est de l’Algérie. L’étude pétrographique montre que le massif d’Oued El-Annab se compose principalement de groupe des feldspaths, la biotite est en quartz. Les feldspaths surtout les plagioclases sont les plus abondants et représente presque 50% du massif suivi par la biotite puis le quartz. La spectroscopie infrarouge confirme les résultats pétrographiques et montre que les trois minéraux apparaissent entre le pic 500 et 1500 cm-1 avec des minéraux argileux qui apparaissent après le pic 1000 cm-1 représenté par des pics faibles. Ce massif contient une quantité importante de feldspath peu utiliser en industrie de céramique, de verre et glaçures .

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Belaidi, H., Kitouni, S., & Chellat, S. (2022). LES CARACTÉRISATIONS DES FELDSPATHS DU MASSIF D’OUED EL-ANNAB ET LA POSSIBILITÉ DE LES EXPLOITER POUR L’INDUSTRIE. URBAN ART BIO, 1(3), 1–13. https://doi.org/10.35788/uab.v1i3.49
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