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Table S3: 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

Parameters used in quantitative modelling and results

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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

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

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