Figure F14. Serpentinized peridotite cut by plagioclase-bearing magmatic veins (top and lower left) (interval 210-1277A-9R-1, 1–19 cm). Sparry calcite veins appear at the contacts between the magmatic intrusive rocks and the serpentinites.

Figure F14. Serpentinized peridotite cut by plagioclase-bearing magmatic veins (top and lower left) (interval 210-1277A-9R-1, 1–19 cm). Sparry calcite veins appear at the contacts between the magmatic intrusive rocks and the serpentinites.