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Table S2: 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

Rb–Sr isotopic compositions for the studied syenites

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https://orcid.org/0000-0003-0476-5302

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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

Geological Society, London, Special Publications

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Geology not elsewhere classified

Keywords

Eastern Dharwar Craton Paleoproterozoic Rb breakup supercraton 2.21 Ga mafic dyke swarms syenite metaluminou Superia magmatism implication Geology

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