Redox state of the Dharwar craton root as inferred from eclogite and peridotite sourced mantle cargo, with implications for kimberlite and lamproite magma formation.

Autor:	Shaikh, Azhar M.1,2,3 (AUTHOR) azharms@iiserbpr.ac.in, Bussweiler, Yannick4 (AUTHOR), Viljoen, Fanus2 (AUTHOR), Bolhar, Robert3 (AUTHOR), Ravi, S.5 (AUTHOR), Hezel, Dominik C.6 (AUTHOR), Ueckermann, Henriëtte2 (AUTHOR), Tappe, Sebastian2,7 (AUTHOR)
Zdroj:	Contributions to Mineralogy & Petrology. Dec2023, Vol. 178 Issue 12, p1-19. 19p.
Databáze:	Academic Search Ultimate
Externí odkaz:	Zobrazit plný text záznamu Full text from SpringerLink