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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 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 TiO
2
(wt%) v. (a) K
2
O (wt%), (b) Na
2
O (wt%), (c) SiO
2
(wt%), (d) Al
2
O
3
(wt%), (e) Th (ppm) and (f) U (ppm) for the studied syenites
History
ORCID FOR SUBMITTING AUTHOR(s)
https://orcid.org/0000-0003-0476-5302
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Geology not elsewhere classified
Keywords
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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CC BY 4.0
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