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Table S1: Paleoproterozoic metaluminous syenites synchronous with the c. 2.21 Ga mafic dyke swarms from the Eastern Dharwar Craton, India: implications for alkaline magmatism associated with the breakup of supercraton Superia

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posted on 21.01.2021, 09:57 authored by Ashutosh Pandey, N.V. Chalapathi Rao, Waliur Rahaman, Vikas Seth, Samarendra Sahoo
Representative mineral composition data from the studied syenites

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