B. Madeddu et al., POSTPLIOCENE STRESS-FIELD AND PRESENT-DAY STRAINS IN THE SOUTHWESTERNALPS, Bulletin de la Societe geologique de France, 167(6), 1996, pp. 797-810
A detailed analysis of 16 new earthquake mechanisms, followed by a syn
thesis of all available focal solutions in the southwestern Alps, allo
ws to characterize the various present-day deformation regimes within
the pre-Triassic basement of this region. We define 4 areas of deforma
tion, 3 of which are mainly compressional and one of which is extensio
nal (Haute-Ubaye region). The use of microtectonic data, which provide
s information about stress state in the sedimentary cover, and the ana
lysis of P-axes and T-axes directions of the focal solutions, allow to
discuss the present-day stress field in this region. We show the vari
ation of stress field directions which are NE-SW in the Brianconnais u
nits, N-S in the Digne region and NW-SE in the south south-east of the
Argentera massif and in the Ligurian basin. On the basis of these ana
lyses we discuss the present-day kinematic relationships between the w
estern Alps and the Ligurian Basin, in the framework of the NW-SE conv
ergence between the European and African plates. We then examine wheth
er or not previously published late Tertiary geodynamic models are sti
ll appropriate for the present-day tectonics in the southwestern Alps.