Archean to Proterozoic (3535–900 Ma) crustal evolution of the central Aravalli Banded Gneissic Complex, NW India: New constraints from zircon U-Pb-Hf isotopes and geochemistry
Parampreet Kaur, Armin Zeh, Naveen Chaudhri
Topics & Concepts
ZirconGeochemistryGeologyArcheanProterozoicPartial meltingGranuliteFelsicCrustPetrologyUnderplatingMaficSupercontinentContinental crustCratonLithosphereGeomorphologyPaleontologyTectonicsFaciesStructural basinGeological and Geochemical Analysisearthquake and tectonic studiesHigh-pressure geophysics and materials