Phase Relations in the Fe–S–C System at P = 0.5 GPa, T = 1100–1250°C: Fe–S–C Liquation and Its Role in the Formation of Magmatic Sulfide Deposits
Crossref DOI link: https://doi.org/10.1134/S1028334X21030028
Published Online: 2021-04-14
Published Print: 2021-03
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Gorbachev, N. S.
Shapovalov, Yu. B.
Kostyuk, A. V.
Gorbachev, P. N.
Nekrasov, A. N.
Soultanov, D. M.
Text and Data Mining valid from 2021-03-01
Version of Record valid from 2021-03-01
Article History
Received: 19 November 2020
Revised: 2 December 2020
Accepted: 3 December 2020
First Online: 14 April 2021