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We describe the textural evolution of chromites from the Neoarchaean Sittampundi anorthosite complex in southern India. A series of micro‐structural developments in chromites with increasing temperature is recorded. The intracrystalline deformation started with a high strain rate at elevated temperature. At higher temperature, crystal plastic deformation like recovery/recrystallization was initiated...
Chrome-spinels of anorthosite-hosted chromitite bodies from Sittampundi layered igneous complex, southern India, metamorphosed under eclogite-facies condition have been studied. Besides anorthosites as the dominant rock type discontinuous layers of peridotite, pyroxenite and lenses of gabbroic granulite/eclogite occur at the bottom of the complex. Chromite grains are deformed exhibiting features of...
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