Cite
The Formation of Magnesite Ores by Reactivation of Dunite Channels as a Key to Their Spatial Association to Chromite Ores in Ophiolites: An Example from Northern Evia, Greece.
MLA
Grieco, Giovanni, et al. “The Formation of Magnesite Ores by Reactivation of Dunite Channels as a Key to Their Spatial Association to Chromite Ores in Ophiolites: An Example from Northern Evia, Greece.” Minerals (2075-163X), vol. 13, no. 2, Feb. 2023, p. 159. EBSCOhost, https://doi.org/10.3390/min13020159.
APA
Grieco, G., Cavallo, A., Marescotti, P., Crispini, L., Tzamos, E., & Bussolesi, M. (2023). The Formation of Magnesite Ores by Reactivation of Dunite Channels as a Key to Their Spatial Association to Chromite Ores in Ophiolites: An Example from Northern Evia, Greece. Minerals (2075-163X), 13(2), 159. https://doi.org/10.3390/min13020159
Chicago
Grieco, Giovanni, Alessandro Cavallo, Pietro Marescotti, Laura Crispini, Evangelos Tzamos, and Micol Bussolesi. 2023. “The Formation of Magnesite Ores by Reactivation of Dunite Channels as a Key to Their Spatial Association to Chromite Ores in Ophiolites: An Example from Northern Evia, Greece.” Minerals (2075-163X) 13 (2): 159. doi:10.3390/min13020159.