TRACK experiment

Guilhem Barruol &
Seismic velocity tomography, geodynamic modelling and geochemical characterictics of the tertiary and quaternary volcanic activity provide an evidence for the ascent of a mantle plume beneath the MC during Tertiary. To characterize the pervasive upper mantle structures and the upper mantle flow beneath the French Massif Central, we deployed 25 three component stations (short period, intermediate and broad-band) during the period 1998-1999 in the southern Massif central, from the Clermont Ferrand volcanic area to the...
1 citation reported since publication in 2011.
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