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Fig. 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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journal contribution
posted on 21.01.2021, 09:57 by Ashutosh Pandey, N.V. Chalapathi Rao, Waliur Rahaman, Vikas Seth, Samarendra Sahoo
Bivariate plot with relatively immobile component TiO2 (wt%) v. (a) K2O (wt%), (b) Na2O (wt%), (c) SiO2 (wt%), (d) Al2O3 (wt%), (e) Th (ppm) and (f) U (ppm) for the studied syenites

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