RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES1004, doi:10.2205/2015ES000550, 2015
Compo- | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 | 13 | 14 |
nent | ||||||||||||||
$\mathrm{SiO_2}$ | 35.46 | 37.07 | 37.33 | 36.62 | 37.41 | 37.53 | 36.94 | 37.87 | 36.57 | 38.97 | 38.91 | 37.68 | 39.98 | 41.0–42.7 |
$\mathrm{TiO_2}$ | 5.45 | 2.30 | 4.77 | 1.20 | 5.91 | 6.23 | 2.70 | 2.66 | 9.20 | 2.86 | 3.67 | 5.53 | 9.13 | 1.07–1.59 |
$\mathrm{Al_2O_3}$ | 16.58 | 17.46 | 16.12 | 17.30 | 16.74 | 16.76 | 17.03 | 16.40 | 15.84 | 13.80 | 14.62 | 16.18 | 13.45 | 11.7–13.2 |
$\mathrm{Cr_2O_3}$ | 0.19 | 0.05 | 0.60 | 0.32 | 0.19 | 0.35 | 0.07 | 0.70 | – | 0.15 | 0.17 | 0.43 | 0.71 | 0.19–0.81 |
FeO* | 15.35 | 11.78 | 14.30 | 10.91 | 6.91 | 6.71 | 8.32 | 5.46 | 12.82 | 8.18 | 9.88 | 9.72 | 3.57 | 2.72–4.57 |
MnO | 0.03 | 0.12 | 0.50 | 0.13 | 0.07 | 0.05 | 0.10 | 0.02 | – | 0.04 | 0.05 | 0.01 | 0.04 | 0.0–0.5 |
MgO | 13.64 | 17.82 | 15.66 | 19.78 | 18.40 | 18.41 | 19.62 | 21.96 | 12.87 | 19.44 | 17.72 | 17.53 | 18.73 | 23.9–25.5 |
CaO | 0.13 | 0.00 | 0.00 | 0.00 | 0.03 | 0.05 | 0.11 | 0.07 | – | – | 0.07 | 0.04 | – | 0.05 |
$\mathrm{Na_2O}$ | 1.30 | 1.97 | 0.94 | 2.34 | 0.56 | 0.61 | 0.46 | 0.13 | 1.11 | 0.49 | 0.30 | 0.52 | 0.06 | 0.17–0.43 |
$\mathrm{K_2O}$ | 8.72 | 8.48 | 8.56 | 9.53 | 9.83 | 9.73 | 10.05 | 10.32 | 8.92 | 9.51 | 9.83 | 9.46 | 9.64 | 9.27–9.97 |
Note: the Roca Negra: 1 – average biotite composition (9 analyses); 2 – average phlogopite composition (4 analyses); 3, 4 – phlogopite [Sanchez, 1983], 5–7 – central Spain, 5 – average phlogopite composition in glimmerites (10 analyses), 6 – average phlogopite composition in spinel lherzolites (5 analyses), [Ancochea and Nixon, 1987], 7, 8 – phlogopite in phlogopite pyroxenite xenoliths from Roccamonfina volcano, Italy (7 and 5 analyses) [Giannetti and Luhr, 1990], 9 – phlogopite in spinel lherzolite xenolith in basalts at the Bartoi River, Baikal Rift, Russia [Ionov and Hofmann, 1995], 10 – phlogopite in glimmerite in peridotite from the Bohemian Massif [Becker et al., 1999], 11 – phlogopite in xenolith form the Roberts Victor kimberlite pipe [MacGregor, 1979], 12 – xenolith of micaceous websterite [Lasko and Sharkov, 1988], 13 – garnet peridotite, Tanzania [Dawson, 1972], 14 – variations in mica composition in metasomatic zones in peridotites [Dawson and Smith, 1977]. |
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.