Le site des “Dix-Neuf” à Lauwin-Planque (Nord). Un établissement rural du IIe s.

in Leroy, Emmanuelle (Ed.) Du Néolithique aux Temps modernes. 40 ans d’archéologie territoriale. Mélanges offerts à Pierre Demolon (2012)

Site directed mutagenesis as applied to psychrophilic alpha-amylase

Conference (2000)

Le site du Trou Al'Wesse (comm. de Modave) : Campagne de Fouille 2004

in Notae Praehistoricae (2004), 24

We present the discovery context of Neolithic ceramic sherds from stratum 4 (attributed to the Late Mesolithic) at Trou Al'Wesse. The spatial distribution of the archaeological materials, as well as ... [more ▼]

We present the discovery context of Neolithic ceramic sherds from stratum 4 (attributed to the Late Mesolithic) at Trou Al'Wesse. The spatial distribution of the archaeological materials, as well as stratigraphic data, demonstrate that these sherds are not associated with the Mesolithic assemblage. Thestratigraphy also shows that, near the cliff face, there is no mixing between the two occupations. [less ▲]

Site effect analysis around the seismically induced Ananevo, Rockslide, Kyrgyzstan

in Bulletin of the Seismological Society of America (2002), 92(8), 3190-3209

In 1911, the surface-wave magnitude 8.2 Kemin earthquake hit northeastern Tien Shan (Kyrgyzstan), close to the cities of Bishkek and Almaty, the capitals of Kyrgyzstan and Kazakhstan, respectively ... [more ▼]

In 1911, the surface-wave magnitude 8.2 Kemin earthquake hit northeastern Tien Shan (Kyrgyzstan), close to the cities of Bishkek and Almaty, the capitals of Kyrgyzstan and Kazakhstan, respectively. Several hundreds of people were killed by the earthquake, some by indirect effects such as landslides and mudflows. A particular but nonfatal landslide triggered by the Kemin event was a rockslide in the vicinity of Ananevo, north of lake Issyk Kul (Kyrgyzstan) rockslide located above the fault zone activated in 1911. In the summer of 1999, a geophysical-seismological field trip was organized to study geology and to record seismic ground motions on and around the Ananevo rockslide. The work was part of project assessing seismogenic landslide hazard in northern Kyrgyzstan, based on various case studies of slope failures in connection with site-specific ground-motion dynamics. The geophysical investigations consisted of seismic refraction tests processed as 2D seismic tomographies and surface-wave inversion, which were combined to build a 3D geophysical model of the landslide site. Ground motions from small earthquakes were analyzed using several techniques to define site effects over the mountain massif. Both H/V and standard spectral ratios indicated lower dominant frequencies with stronger amplification in the crest region with respect to the mountain slope. These effects could be partially simulated by I D, 2D, and 3D finite-element modeling. By comparing the numerical results with the experimental data, the presence of a surficial low-velocity layer of varying thickness appeared to be the key factor controlling the ground motion around the rockslide. [less ▲]

Le site et la fouille

in Akkadica (1992), 79-80

Site Index Curves For Alnus Glutinosa (L.) Gaertn. In Southern Belgium: Effect Of Site On Curve Shape

in Forestry (2004), 77(2), 157-171

Site index curves were developed for Alnus glutinosa (L.) Gaertn. in southern Belgium. Five models of Duplat and Tran-Ha were fitted to a data set of 15 stem analyses divided into two data subsets clearly ... [more ▼]

Site index curves were developed for Alnus glutinosa (L.) Gaertn. in southern Belgium. Five models of Duplat and Tran-Ha were fitted to a data set of 15 stem analyses divided into two data subsets clearly characterized by different height growth patterns. Model III was found to fit data sets best, both separately and combined. Various statistical comparisons made between the two curve sets underline shape variations corresponding to different soil conditions. A comparison between Belgian and other European curves highlights the effect of the soil on growth curve shape, which is at least as important as that of climatic factors. However, for practical reasons, the use of a general global model, which does not specifically take into account differences in height growth patterns, is satisfactory for productivity evaluation and is recommended for forest management. [less ▲]

Le site Néolithique final de Labarthe 2 à Argelos (Pyrénées Atlantiques) : une occupation temporaire ?

in Perrin, Thomas; Sénépart, Ingrid; Thirault, Eric (Eds.) Actes des 9ème Rencontres Méridionales de Préhistoire récente, St-Goerges-de-Didonne (17), 08 et 09 octobre 2010 (2012)

In the Luy de France valley at Labarthe-Argelos (Pyrénées-Atlantiques), a rescue excavation was carried out during spring 2009 on a surface of 2200 m2. The entire Final Neolithic remains were recovered ... [more ▼]

In the Luy de France valley at Labarthe-Argelos (Pyrénées-Atlantiques), a rescue excavation was carried out during spring 2009 on a surface of 2200 m2. The entire Final Neolithic remains were recovered from one single soil unit within the colluvium sequence at bottom of the slope. Nine hearths have been studied (see contribution of B. Nicolle, this volume), the pottery and lithic objects have been positioned in the stratigraphy and a delimitated area with abundant pottery sherds has been identified in close proximity to a small hearth. The pottery assemblage can be assigned to the Final Neolithic sequence of south-western France, within the third millennium. It forms, however, an original facies and contributes to fill an information gap in the Northern Pyrenean region. The lithic artefacts were made on flint and quartzite. Two radiocarbon dates consistent with the data assemblage stemming from the excavation place these occupations between 2600 and 2400 BC cal. The field data attribute Labarthe 2 to a series of small sites exhibiting subtle features not very deeply anchored into the ground that are known in the Bearn and the Landes regions. They are interpreted by a variety of hypotheses: stops during pastoral displacements, crossing points of the valley, places for specific activities (fishing, hunting?), etc. Their location, at the foot of a spur dominating the confluence may also be complementary of a possible settlement on top of the spur. [less ▲]

Le site préhistorique du Trou Al’Wesse à Modave

Book published by Derouaux (2005)

Site Web du cours "Fédéralisme comparé"

Learning material (n.d.)

Site Web du cours "Introduction aux comportements politiques"

Learning material (n.d.)