Abstract

"A series of charnockitic rocks and associated cordierite-bearing rocks from Western Australia has been described and compared with charnockitic rocks from other localities. This charnockitic suite is considered to be a series of basic intrusions into an older series of paraschists.... In view of the similarity to the Indian and Antarctic charnockites it appears possible that the charnockitic rocks of these areas are of similar origin and that charnockite... rather than being the result of crystallization from a magma, is due to the granitization of older hypersthene-bearing rocks."

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