U–Pb Geochronology and Petrogenesis of Dongargarh Granite, Bastar Craton, Central India: Insights Into Crustal Growth and Critical Metals Mineralization Across Archean‐Proterozoic Transition Dongargarh granite formed due to partial melting of Neoarchean lower crust through intracrustal recycling, with variable contributions from TTGs, metasediments, and upper mantle. Dongargarh…

Research : doi.org/10.1002/gj.7...
wiley

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