Characterization of the mantle & its evolution during the Archean-Proterozoic are essential to understand early earth geodynamic conditions. It has been established that the crust of Early earth formed due to the partial melting of the mantle. The Pr
Section: Earth, Atmosphere & Environment Sciences (Research Project)
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Proterozoic mantle
Proterozoic mantle evolution: Dharwar and Bastar connection
Research Project › Earth, Atmosphere & Environment Sciences
Physicochemical conditions
Physicochemical conditions of the kimberlite factory: A mineral-chemical approach to trace magmatic evolution from Earth's mantle to the surface
Research Project › Earth, Atmosphere & Environment Sciences
Initiation from
Initiation from stagnant-lid to modern day Plate Tectonics: Constraints from Interleaved Eoarchean Gneisses and Charnockites in the west Bastar Craton
Research Project › Earth, Atmosphere & Environment Sciences
Detrital zircon
Detrital zircon evidence for Eoarchean to Mesoarchean Crustal evolution dichotomy: The stagnant lid vs. mobile lid geodynamic regime
Research Project › Earth, Atmosphere & Environment Sciences
Geochemical and
Geochemical and Petrological Study of eruptible and non-eruptible large silicic magma Systems in reference to the LIP Bijli rhyolite near Amgaon (Maharashtra) and Bundelkhand granitoid and associated Quartz reefs near Babina (Uttar Pradesh)
Research Project › Earth, Atmosphere & Environment Sciences