Evidence for a Paleoproterozic event of metamorphism in the Bastar craton, Central India: P-T-t constraints from mineral chemistry and U-Pb geochronology of mafic dykes | Zendy

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Evidence for a Paleoproterozic event of metamorphism in the Bastar craton, Central India: P-T-t constraints from mineral chemistry and U-Pb geochronology of mafic dykes

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