The Stability of NRM of Deccan Traps Basalts in India

Abstract
Samples of Deccan Trap basalts from all flows in the Mahabaleshwar and Amboli cliff sections in western India have been analysed by the thermomagnetic, and X-ray techniques. The principal conclusions are: 1) the NRM was stablized by oxidation of titanomagnetite shortly after eruption of lavas; 2) low-temperature oxidation of titanomagnetite can occur at ordinary temperatures is within a million years.

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