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Economic Geology; May 1966; v. 61; no. 3; p. 555-562
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Coexisting iron-titanium oxide minerals in norites associated with anorthosites of Bengal, India

Mihir K. Bose, and Asit K. Roy

The characteristic assemblage in ore pockets within reconstituted norites is ferrian ilmenite-ilmenomagnetite-spinel. The xenoblastic texture suggests that of many high-grade metamorphic rocks. The field associations, mineralogic assemblage, and composition of individual phases indicate a magmatic origin. The ores probably represent magmatic segregations metamorphosed under granulite facies conditions.

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