R
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Last name: RÉGNIER
First name: Marc
International audience
International audience
We analyzed interseismic velocity fields along the Vanuatu arc subduction zone from more than 45 GPS station measurements spanning 15 years. Convergence with respect to the Australian plate (AP) is normal to the trench, with amplitudes that vary greatly from a maximum of 170 mm a−1 at Vanikoro to 27 mm a−1 facing the D'Entrecasteaux Ridge...
International audience
The offshore Tumbes-Guayaquil forearc basin in the accretionary prism of Northern Peru-Southern Ecuador shows evidence of gravity-driven large-scale deformation systems active during the Late Neogene-Quaternary period. Subsurface data and the construction of eight structural cross-sections show that the ~8 km-thick Oligocene-Quaternary...
International audience
The analysis of the seismicity catalog (1996 to 2019) covering the region from the Juramountains to Corsica provides a first-order image of the distribution of earthquakes, highlightinglarge structures such as the Briançonnais and Piedmontais seismic arcs, the eastward deepeningof the focal depths through the Western Alps, several large active...
International audience
International audience
The southern Ecuadorian forearc system is related to the subduction of the oceanic Farallon/Nazca Plate beneaththe continental South American Plate since the Late Cretaceous, and currently evolves with the dynamic of atectonic block called North Andean Sliver. To explore the structural architecture and processes controlling theUpper...
The Mw7.8 Pedernales earthquake is associated with the subduction of the Nazca Plate beneath the South American Plate. The mainshock caused many casualties and widespread damages across the Manabi province. The 150 km-long coseismic rupture area is found beneath the coastline, near 25 km depth. The rupture propagated southward and involved the...