Reply to the comment on “Ti-poor high-Al chromitites of the Moa-Baracoa ophiolitic massif (eastern Cuba) formed in a nascent forearc mantle” by Rui et al. [Ore Geol. Rev., 104847]
Author:
Funder
National Natural Science Foundation of China
Publisher
Elsevier BV
Subject
Economic Geology,Geochemistry and Petrology,Geology
Reference27 articles.
1. Formation and modification of chromitites in the mantle;Arai;Lithos,2016
2. Rates and mechanisms of Fe–Mg interdiffusion in olivine at 980–1300 ℃;Chakraborty;J. Geophys. Res.: Solid Earth,1997
3. Calcium amphibole exsolution lamellae in chromite from the Semail ophiolite: evidence for a high-pressure origin;Chen;Lithos,2019
4. Colás, V., González-Jiménez, J.M., Camprubí, A., Griffin, W., Proenza, J., Centeno-Garcia, E., O'Reilly, S., Garcia-Casco, A., Belousova, E., Talavera, C., Farré de Pablo, J., Satsukawa, T., 2020. The recycling of chromitites in the Puerto Nuevo ophiolite (Baja California Sur, Mexico). GSA 2020 Connects Online. 10.1130/abs/2020AM-359233.
5. The recycling of chromitites in ophiolites from southwestern North America;González-Jiménez;Lithos,2017
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