Late Pleistocene folding above the Mail Arrouy Thrust, North-Western Pyrenees (France)
Résumé
The Western Pyrenees have experienced several major earthquakes in the last 400. years. Herein, we investigate the ongoing tectonic activity of the Arudy area affected by one of the largest earthquakes (M = 5.1; 1980) registered in the instrumental seismicity catalogue in the Western Pyrenees. Folding of alluvial terraces younger than 17 +/- 3. ky above the Mail Arrouy Thrust (MAT), Attest from a Late Pleistocene tectonic activity. This deformation resulted in a shallow fold with a wavelength of 2800. m and amplitude of 7 to 8. m. The MAT is rooted above a former normal fault of the Cretaceous Iberian margin, which is a potential seismogenic source.Such observations suggest that the northern flank of the Western Pyrenees is still subjected to shortening in response to a compressional stress regime. This compression is consistent with the African-Eurasian plate kinematics and the Arudy 1980 earthquake. Nonetheless, recent seismological data suggest the presence of an extensional stress regime in the range. This extension is indicated by some seismic events mostly observed in the Pyrenean high chain. Our hypothesis is that these extension-driven events could be due to a local stress-field induced by the elevation of the range. On the contrary, the compression, associated with the regional stress regime, could prevail in the outermost domain of the range.
Mots clés
Neotectonic
Pleistocene
Pyrenees
Seismic risk
Seismogenetic sources Compressional
Extensional stress
Late Pleistocene
Normal faults
Plate kinematics
Seismic event
Seismological data
Stress regime
Tectonic activity Engineering controlled terms: Tectonics Engineering main heading: Earthquakes GEOBASE Subject Index: deformation
earthquake
earthquake catalogue
folding
neotectonics
normal fault
plate tectonics
seismicity
seismology
tectonic phenomena
thrust Regional Index: Pyrenees