Analyses of the stress field in southeastern France from earthquake focal mechanisms

Owing to the apparent deformation field heterogeneity, the stress regimes around the Provence block, from the fronts of the Massif Central and Alpine range up to the Ligurian Sea. have not been well defined. To Improve the understanding of the SE France stress field, we determine new earthquake focal mechanisms and compute the present-day stress states by inversion of the 89 available focal mechanisms around the Provence domain, including 17 new ones calculated in the current study. This study provides evidence of six distinct deformation domains around the Provence block, with different tectonic regimes. On a regional scale, we identify three zones characterized by; significantly different stress regimes: a western one affected by an extensional stress (normal faulting) regime. a southeastern one characterized by a compressional stress (reverse to strike-slip Faulting) regime with NNW- to WNW-trending sigma (1); and a northeastern one, namely the Dine nappe front, marked by a NE-trending compression. Note that the Digne nappe back domain is controlled by an extensional regime that is deforming the western Alpine core. This extensional regime could br a response to buoyancy forces related to the Alpine high topography. The stress regimes in the southeast of the Argentera Massif and around the Durance fault are consistent with a coherent NNW-trending sigma (1), implying a left-lateral component of the active reverse oblique slip of the Moyenne Durance Fault. In the Rhone Valley. an E-trending extension characterizes the tectonic regime, implying a normal component of the present-jay Nimes fault displacement. This study provides evidence for short-scale variation of the stress states, which arises from abrupt changes in the boundary force influences on upper crustal fragments (blocks). These spatial stress changes around the Provence block result from the coeval influence of forces applied at both its extremities. namely in the northeast the Alpine front push. and in the southeast the northward African plate drift. In addition to these boundary forces. the mantle plume under the Massif Central influences the western block boundary.