Fluid-magma decoupling in a hot-spot volcano

Melt and fluid inclusions in olivines from the last 1998 eruption of Piton de la Fournaise (PdF), have recorded a range of volatile partial pressures (350-420 MPa), the highest, so far for this volcano, are found in Fo-rich o livines from a vent remote from the main eruptive activity. Such pressures indicate that fractionation of olivine (and other crystals) occur below the crust-mantle 'boundary in a CO2-rich volatile saturated environment. Toget her with previously published data, the model that emerges for PdF is one w here olivines which have crystallized from multiple past magma injection ev ents [see Albarede et al., 1997], may be picked up by newly intruding magma , anywhere from upper-mantle depths to the surface.,This model is likely to apply to other shield volcanoes. Magma production and transport to the sur face is accompanied by continuous open-system degassing through the permeab le volcanic pile. The calculated H2O content of primary basalts (MgO approx imate to 12-14 wt.%) from PdF may reach 0.7-1 wt.% implying a rather H2O-ri ch hot spot mantle source.