RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES1004, doi:10.2205/2015ES000550, 2015
| Component | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 |
| $\mathrm{SiO_2}$ | 0.39 | 0.50 | 0.70 | 0.41 | 0.38 | - | 0.57 | - | 0.44 | 0.39 |
| $\mathrm{TiO_2}$ | 9.81 | 6.42 | 7.58 | 7.46 | 21.28 | 2.92 | 2.80 | 0.66 | 1.06 | 1.76 |
| $\mathrm{Al_2O_3}$ | 6.80 | 6.89 | 6.86 | 6.86 | 12.45 | 10.71 | 6.29 | 21.55 | 22.13 | 8.99 |
| FeO* | 77.95 | 78.83 | 80.39 | 81.11 | 58.99 | 80.27 | 86.40 | 68.14 | 67.42 | 84.76 |
| MnO | - | - | - | - | - | 0.61 | - | 0.53 | - | - |
| MgO | 4.64 | 5.22 | 4.13 | 4.07 | 5.78 | 5.15 | 3.57 | 8.20 | 8.67 | 4.34 |
| $\mathrm{Cr_2O_3}$ | - | - | - | - | 0.88 | 0.83 | - | - | - | - |
Citation: Grachev A. F. (2015), Pyroxenite xenoliths in basalts of the Roca Negra volcano, Catalonia, Russ. J. Earth Sci., 15, ES1004, doi:10.2205/2015ES000550.
Copyright 2015 by the Geophysical Center RAS.