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Showing 1 to 1 of 1 for “"Central Maine Trough"”.
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Garnetites of the Cardigan Pluton - Evidence for Restite and Implications for Source Rock Compositions.
… melting of a calc-pelitic metasediment from the Central Maine trough could have generated a granodioritic melt similar to the average granodiorite of the Cardigan pluton. However, most of the Cardigan garnetite rocks appear to have been derived from pelites, as they are too poor in CaO and Na2O. …