Neoarchean deep subduction (>200 km) due to the Wilson-cycle type plate tectonics: Evidence from coesite and supersilicic K-pyroxene in diamondiferous kimberlite-borne eclogite xenolith from Dharwar craton, India - Garnet and clinopyroxene data

Name: Neoarchean deep subduction (>200 km) due to the Wilson-cycle type plate tectonics: Evidence from coesite and supersilicic K-pyroxene in diamondiferous kimberlite-borne eclogite xenolith from Dharwar craton, India - Garnet and clinopyroxene data
Creator: Amitava Chatterjee
Published: 2021-12-13T16:29:45.330Z
Keywords: Mineral Chemistry, Garnet

Chatterjee, Amitava; Chalapathi Rao, N.V.; Pandey, Rohit; Pandey, Ashutosh

doi:10.17632/c2d2tbvfjs.1

Neoarchean deep subduction (>200 km) due to the Wilson-cycle type plate tectonics: Evidence from coesite and supersilicic K-pyroxene in diamondiferous kimberlite-borne eclogite xenolith from Dharwar craton, India - Garnet and clinopyroxene data

Published: 13 December 2021| Version 1 | DOI: 10.17632/c2d2tbvfjs.1

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The Excel files contain mineral chemical data of garnet and clinopyroxene used in Figure 3a and 3b. The word file contains full references of the data used in Figure 3a and 3b.

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Banaras Hindu University

Neoarchean deep subduction (>200 km) due to the Wilson-cycle type plate tectonics: Evidence from coesite and supersilicic K-pyroxene in diamondiferous kimberlite-borne eclogite xenolith from Dharwar craton, India - Garnet and clinopyroxene data

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