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Geothermometric and Oxygen Fugacity Studies of Mayurbhanj Basic Igneous Complex
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The basic igneous complex of Mayurbhanj is a differentiated suite composed of harzburgite, gabbronorite, leucogabbronorite and anorthosite. EPMA of the coexisting oxides in the rock samples reveal that magnetite-ilmenite have re-equilibrated between 770°C and less than 500°C and fo2, of 10-16 to less than 10-25. Ilmenite granules and thick lamellae have identical composition and approach pure FeTiO3. The chrominn spinel-olivine geothermometry in harzburgite suggests a temperature of 1263°C. The pyroxene geothermometric data in gabbroic rocks indicate equilibration temperature range of 819° C to 1071° C. The thermometric data indicate that the magnetite and ilmenite equilibrated at lower temperature than the coexisting pyroxenes for a particular rock sample.
Keywords
Igneous Petrology, Basic Igneous Complex, P-T Conditions, Oxygen Fugacity, Orissa.
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