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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 2021-01-21, 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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ORCID FOR SUBMITTING AUTHOR(s)
https://orcid.org/0000-0003-0476-5302
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Geology not elsewhere classified
Keywords
Eastern Dharwar Craton
Paleoproterozoic
breakup
2.21 Ga mafic dyke swarms
syenite
metaluminou
supercraton Superia Representative ...
magmatism
implication
Geology
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CC BY 4.0
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