Nicolas d'Oreye

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Continental rifts begin and develop through repeated episodes of faulting and magmatism, but strain partitioning between faulting and magmatism during discrete rifting episodes remains poorly documented. In highly evolved rifts, tensile stresses from far-field plate motions accumulate over decades before being released during relatively short time intervals(More)
1 Dept. of Geology, Royal Museum for Central Africa, Leuvensesteenweg 13, 3080 Tervuren, Belgium, christelle.wauthier@africamuseum.be 2 Dept. ArGEnCo, University of Liège, Sart Tilman B52, 4000 Liège, Belgium 3 Lab. Magmas et Volcans, Université Blaise Pascal – UMR 6524, rue Kessler 5, 63038 ClermontFerrand, France 4 Centre d’Informations Géographiques(More)
1. Lab. Magmas et Volcans, Université Blaise Pascal – UMR 6524, 5 rue Kessler, 63038 ClermontFerrand, France, V.Cayol@opgc.univ-bpclermont.fr 2. Dept. of Geophysics/Astrophysics, National Museum of Natural History, Rue Josy Welter 19, 7256 Walferdange, Luxembourg, 3. Dept. of Geology, Royal Museum for Central Africa, Leuvensesteenweg 13, 3080 Tervuren,(More)
Radar interferometry has proven to be a very suitable, low-cost and accurate tool to measure surface displacements. We investigate several data fusion or time-series analysis strategies which aim to mitigate C-band InSAR restrictions for volcano deformation monitoring applications. The focus is on active African volcanic areas. Firstly, data fusion of(More)
1 Dept. of Geology, Royal Museum for Central Africa, 3080 Tervuren, Belgium, christelle.wauthier@africamuseum.be 2 Dept. ArGEnCo,University of Liège, Sart Tilman B52, 4000 Liège, Belgium 3 Delft Inst. of Earth Obs. and Space Systems, Delft Univ. of Tech., 2629HS Delft, The Netherlands 4 Dept. of Geophysics/Astrophysics, National Museum of Natural History,(More)
A summit and upper flank eruption occurred at Nyamulagira volcano, Democratic Republic of Congo, from 2–27 January 2010. Eruptions at Nyamulagira during 1996–2010 occurred from eruptive fissures on the upper flanks or within the summit caldera and were distributed along the ~N155E rift zone, whereas the 2011–2012 eruption occurred ~12 km ENE of the summit.(More)
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