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Exploitation of malaya garnet in eluvium in 1998, in a  broken up leptynite
Leptynites with amphibolo-pyroxenite intercalation often with rutile and graphite abound in certain areas in  Madagascar. Leptynites derive from granites by disappearance of mica; the garnetiferous mica schists constitute the opposed pole in which biotite prevails, with progressive disappearance of feldspar.
    
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