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Article Reference Sédimentologie et Coraux du bioherme de marbre rouge frasnien ("F2j") de Tapoumont (Massif de Philippeville, Belgique)
Located in Library / RBINS Staff Publications 2016
Article Reference Sédimentologie et Ostracodes de la limite Eifelien-Givetien à Resteigne (bord sud du Bassin de Dinant, Belgique)
Located in Library / RBINS Staff Publications
Article Reference Sédimentologie et paléoécologie de trois niveaux récifaux du Givetien inférieur de Resteigne (bord sud du Bassin de Dinant, Belgique)
Located in Library / RBINS Staff Publications 2016
Article Reference Sédimentologie et paléoécologie de l'Emsien supérieur et de l'Eifelien inférieur des régions de Couvin et de Villers-la-Tour (bord sud du Synclinorium de Dinant, Belgique)
Located in Library / RBINS Staff Publications
Article Reference Sédimentologie, diagenèse et stratigraphie des biohermes de marbre rouge de la partie supérieure du Frasnien belge. Compte rendu de la Session extraordinaire des Sociétés géologiques belges les 14 et 15 septembre 1990
Located in Library / RBINS Staff Publications 2016
Article Reference Sedimentology, conodonts and ostracods of the Devonian-Carboniferous strata of the Anseremme railway bridge section, Dinant Basin, Belgium.
Located in Library / RBINS Staff Publications
Article Reference Seed dispersal by western lowland gorillas (G. g. gorilla) in south east Cameroon
Located in Library / RBINS Staff Publications
Article Reference Segmented worms (Phylum Annelida): a celebration of twenty years of progress through Zootaxa and call for action on the taxonomic work that remains
Located in Library / RBINS Staff Publications 2021
Article Reference Seismic stratigraphy of the late Quaternary sedimentary infill of Lac d’Armor (Kerguelen archipelago): a record of glacier retreat, sedimentary mass wasting and southern Westerly intensification.
Lac d'Armor (49°27′S, 69°42′E) is a medium-sized, fjord-type lake located on the ‘Grande Terre’ island of the Kerguelen archipelago. A dense grid of high-resolution reflection seismic profiles was collected from this lake basin. The seismic stratigraphic facies reveal a last deglaciation to Holocene infill comparable to the seismic facies found in other glacigenic lakes all over the world. Remarkable features in the seismic stratigraphy are mounded structures found at the southern edge of both sub-basins. The sediment mounds can be interpreted as sediment drifts created by wind-induced bottom currents. The onset of the build-up of these drifts initiated at some point in the Holocene and indicates a strengthening of the southern Westerlies, which are currently the dominant winds on this island.
Located in Library / RBINS Staff Publications
Article Reference Seismotectonic significance of the 2008-2010 Walloon Brabant seismic swarm in the Brabant Massif (Belgium)
Between 12 July 2008 and 18 January 2010 a seismic swarm occurred close to the town of Court-Saint-Etienne, 20 km SE of Brussels (Belgium). The Belgian network and a temporary seismic network covering the epicentral area established a seismic catalogue in which magnitude varies between ML -0.7 and ML 3.2. Based on waveform cross-correlation of co-located earthquakes, the spatial distribution of the hypocentre locations was improved considerably and shows a dense cluster displaying a 200 m-wide, 1.5-km long, NW-SE oriented fault structure at a depth range between 5 and 7 km, located in the Cambrian basement rocks of the Lower Palaeozoic Anglo-Brabant Massif. Waveform comparison of the largest events of the 2008–2010 swarm with an ML 4.0 event that occurred during swarm activity between 1953 and 1957 in the same region shows similar P- and S-wave arrivals at the Belgian Uccle seismic station. The geometry depicted by the hypocentral distribution is consistent with a nearly vertical, left-lateral strike-slip fault taking place in a current local WNW–ESE oriented local maximum horizontal stress field. To determine a relevant tectonic structure, a systematic matched filtering approach of aeromagnetic data, which can approximately locate isolated anomalies associated with hypocentral depths, has been applied. Matched filtering shows that the 2008–2010 seismic swarm occurred along a limited-sized fault which is situated in slaty, low-magnetic rocks of the Mousty Formation. The fault is bordered at both ends with obliquely oriented magnetic gradients. Whereas the NW end of the fault is structurally controlled, its SE end is controlled by a magnetic gradient representing an early-orogenic detachment fault separating the low-magnetic slaty Mousty Formation from the high-magnetic Tubize Formation. The seismic swarm is therefore interpreted as a sinistral reactivation of an inherited NW–SE oriented isolated fault in a weakened crust within the Cambrian core of the Brabant Massif.
Located in Library / No RBINS Staff publications