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

Pandey, Ashutosh; Rao, N.V. Chalapathi; Rahaman, Waliur; Seth, Vikas; Sahoo, Samarendra

doi:10.6084/m9.figshare.13621823.v1

sp513-2020-92_si_004.pdf (1.34 MB)

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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posted on 2021-01-21, 09:57 authored 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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Eastern Dharwar Craton ppm K 2 O Al 2 O 3 SiO 2 Na 2 O wt 2.21 Ga mafic dyke swarms syenite immobile component TiO 2 supercraton Superia Bivariate plot Geology

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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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