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Greece | |
| Tsikouras, Basilios, Elena Ifandi, Sofia Karipi, Tassos A. Grammatikopoulos, and Konstantin Hatzipanagiotou. (2016) "Investigation of Platinum-Group Minerals (PGM) from Othrys Chromitites (Greece) Using Superpanning Concentrates" Minerals 6, no. 3: 94. https://doi.org/10.3390/min6030094 |
| Tsoupas, G., & Economou-Eliopoulos, M. (2008). High PGE contents and extremely abundant PGE-minerals hosted in chromitites from the Veria ophiolite complex, northern Greece. Ore Geology Reviews, 33(1), 3-19. Zaccarini F, Economou-Eliopoulos M, Kiseleva O, Garuti G, Tsikouras B, Pushkarev E, Idrus A. Platinum Group Elements (PGE) Geochemistry and Mineralogy of Low Economic Potential (Rh-Pt-Pd)-Rich Chromitites from Ophiolite Complexes. Minerals. 2022 12(12):1565. https://doi.org/10.3390/min12121565 |
| Zaccarini F, Economou-Eliopoulos M, Kiseleva O, Garuti G, Tsikouras B, Pushkarev E, Idrus A. Platinum Group Elements (PGE) Geochemistry and Mineralogy of Low Economic Potential (Rh-Pt-Pd)-Rich Chromitites from Ophiolite Complexes. Minerals. 2022 12(12):1565. https://doi.org/10.3390/min12121565 |
| Zaccarini F, Economou-Eliopoulos M, Kiseleva O, Garuti G, Tsikouras B, Pushkarev E, Idrus A. Platinum Group Elements (PGE) Geochemistry and Mineralogy of Low Economic Potential (Rh-Pt-Pd)-Rich Chromitites from Ophiolite Complexes. Minerals. 2022 12(12):1565. https://doi.org/10.3390/min12121565 |
| Kapsiotis, A. N. (2013). Genesis of chromitites from Korydallos, Pindos Ophiolite Complex, Greece, based on spinel chemistry and PGE-mineralogy. Journal of Geosciences, 58(1), 49-69. Argyrios Kapsiotis, Tassos A. Grammatikopoulos, Basilios Tsikouras and Konstantinos Hatzipanagiotou (2010): Platinum-Group Mineral Characterization in Concentrates from High-Grade PGE Al-rich Chromitites of Korydallos Area in the Pindos Ophiolite Complex (NW Greece). Resource Geology 60, 178-191. |
| Argirios Kapsiotis, Tassos A. Grammatikopoulos, Basilios Tsikouras, Konstantin Hatzipanagiotou, Federica Zaccarini und Giorgio Garuti (2011): Mineralogy, composition and PGM of chromitites from Pefki, Pindos ophiolite complex (NW Greece): evidence for progressively elevated fAs conditions in the upper mantle sequence. Mineralogy and Petrology 101, 129-150. |