Peritectic Reaction of Olivine in the Olivine–Jadeite–Diopside–Garnet–(C–O–H) System at 6 GPa as the Key Mechanism of the Magmatic Evolution in the Upper Mantle
Crossref DOI link: https://doi.org/10.1134/S0016702921080048
Published Online: 2021-09-02
Published Print: 2021-09
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Litvin, Yu. A.
Kuzyura, A. V.
Text and Data Mining valid from 2021-09-01
Version of Record valid from 2021-09-01
Article History
Received: 10 September 2020
Revised: 11 January 2021
Accepted: 8 March 2021
First Online: 2 September 2021