Catalogue d'objets d'art... Vente 30 mars 1840...

[Vente (Art). 1840-03-30. Paris]

Catalogue d'objets d'art... Vente 5 mars 1844...

[Vente (Art). 1844-03-05. Paris]

Notice de tableaux... Vente 11 mars 1844...

[Vente (Art). 1844-03-11. Paris]

Catalogue d'un... mobilier,... objets d'art... Vente... Départ de M. le chevalier J***... 19 mars 1845...

[Vente (Art). 1845-03-19. Paris]

Catalogue de tout le matériel du théâtre du Panthéon... Vente 5 mars 1846...

[Vente (Art). 1846-03-05. Paris]

Galerie du Luxembourg, des Musées, palais et châteaux roy. de France gravée et publiée sous la direction de feu Francisque Noel... Dessins, planches,... Vente 12 mars 1828,...

[Vente (Art). 1828-03-12. Paris]

Notice sur les tableaux... de la vente... 26 mars 1839... après Départ de M. Porel...

[Vente (Art). 1839-03-26. Paris]

Structural analysis of interior layered deposits in north and south Coprates Chasma, Mars

Interior layered deposits within an embayment in the northern as well as near the southern wall of Coprates Chasma in the Valles Marineris, Mars are studied using HRSC, CTX, HiRISE and CRISM data. In the northern embayment, layered deposits outcrop in three separate locations (a western deposit, a central deposit and an eastern deposit). The central layered deposit in the north has a stratigraphic thickness of 2 km. The western layered deposit abuts against the chasma wall appearing to have a relatively un-eroded depositional surface. The eastern deposit is near a landslide scar which appears to have exposed basement layering showing downward displacement. This northern embayment is suggested to have been an ancestral basin. The triangular edged deposit near the southern wall of Coprates Chasma has an elongated mound protruding from the central edge and is suggested to be the outer limits of a fault block which is back rotated 6° south. The rotation may be the result of the Valles Marineris opening.

DEFORMATION OF INTERIOR LAYERED DEPOSITS (ILD) AND THEIR ASSOCIATED LANDFORMS IN WEST CANDOR CHASMA, MARS: IMPLICATIONS FOR THE TIMING OF ILD DEPOSITION

On Mars, interior layered deposits (ILD) provide evidence that water was once stable at the surface of the planet and present in large quantities. In West Candor Chasma, the ILD and their associated landforms record the depositional history of the chasma, and the deformation of those deposits provide insight into the stresses acting on them and the chasma as a whole. The post ILD structural history of West Candor is interpreted by analyzing the spatial relationships and orientation trends of structural features within the ILD. Therecording of stresses through brittle deformation of ILDs implies that the ILD had been lithified before the stress was imposed. Based on the prominent orientation trends of deformation features, the orientation of the stress regime acting upon the ILD appears to be linked to the regime that initially created the chasma-forming faults. An additional minor stress orientation was also revealed and may be related to large structures outside west Candor Chasma. The late depositional history of Ceti Mensa is herein investigated by examining the attributes and spatial relationship between unique corrugated, linear formations (CLF). The CLFs appear to be aeolian in origin but display clear indications of brittle deformation, indicating they have been Iithified. Evidence of lithification and the mineral composition of the surrounding material support the interpretation of circulating water in the area.

STRUCTURAL ANALYSIS, LAYER THICKNESS MEASUREMENTS AND MINERALOGICAL INVESTIGATION OF THE LARGE INTERIOR LAYERED DEPOSIT WITHIN GANGES CHASMA, VALLES MARINERIS, MARS

The interior layered deposit (ILD) in Ganges Chasma, Valles Marineris, is a 4.25 km high mound that extends approximately 110 km from west to east. The deposition, deformation, and erosion history of the Ganges ILD records aids in identifying the processes that formed and shaped the Chasma. To interpret structural and geomorphic processes acting on the ILD, multiple layer attitudes and layer thickness transects were conducted on the Ganges ILD. Mineralogical data was analyzed to determine correlations between materials and landforms. Layer thickness measurements indicate that the majority of layers are between 0.5 m and 4 m throughout the ILD. Three major benches dominate the Ganges ILD. Layer thicknesses increase at the ILD benches, suggesting that the benches are formed from the gradual thickening of layers. This indicates that the benches are depositional features draping over basement topography. Layer attitudes indicate overall shallow dips generally confined to a North-South direction that locally appear to follow bench topography. Layering is disrupted on a scale of 40 m to 150 m in 12 separate locations throughout the ILD. In all locations, underlying layering is disturbed by overlying folded layers in a trough-like geometry. These features are interpreted to have formed as submarine channels in a lacustrine setting, subsequently infilled by sediments. Subsequently, the channels were eroded to the present topography, resulting in the thin, curved layering observed. Data cannot conclusively support one ILD formation hypothesis, but does indicate that the Ganges ILD postdates Chasma formation. The presence of water altered minerals, consistently thin layering, and layer orientations provide strong evidence that the ILD formed in a lacustrine setting.

Geology of Hebes Chasma, Valles Marineris, Mars

Hebes Chasma is an 8 km deep, 126 by 314 km, isolated basin that is partially filled with interior layered deposits (ILD), massive deposits of water altered strata. By analyzing the ILD’s structure, stratigraphy and mineralogy, as well as the perimeter faults exposed in the plateau adjacent to the chasma, the evolution and depositional history of Hebes Chasma is interpreted. Three distinct ILD units were found and are informally referred to as the Lower, Upper and Late ILDs. These units have differing layer thicknesses, layer attitudes, mineralogies and erosional landforms. Based on observations of the plateau, wall morphology and slump blocks within the chasma’s interior, chasma evolution appears to be controlled by cross-faults that progressively detached sections of the wall. A scenario involving the loss of subsurface volume and ash fall events is proposed as the dominant setting throughout Hebes’ geologic history.

Droit civil explique : privileges et hypothéques, commentaire de la loi du 23 mars 1855 sur la transcription en matiere hypothecaire

UANL

La perception de l'URSS dans quatre quotidiens français lors de l'émergence de l'Allemagne nazie, juin 1932 — mars 1934

Les relations franco-soviétiques font l'objet de nouvelles études depuis l'ouverture des archives russes après la chute du communisme au début des années 1990. La présente étude vise à cerner comment la presse française percevait l'URSS et ses relations avec la France entre 1932 et 1934. Cette période est cruciale, car elle correspond à l'arrivée du nazisme en Allemagne et à un certain rapprochement franco-soviétique. La prise du pouvoir par Hitler eut un impact majeur sur les relations entre les deux pays, mais ce ne fut pas toujours compris rapidement en entièrement. Les journaux analysaient la situation avec une perspective compromise par leurs opinions politiques ou leurs intérêts financiers. Néanmoins, nous observons une nette évolution de leurs points de vue sur les 21 mois étudiés ici. Cela est dû à l'aggravation de la menace allemande et à la politique menée par l'URSS et par une partie du corps politique français. Afin d'avoir un échantillon viable, nous nous intéresserons à quatre quotidiens majeurs : Le Figaro, Le Temps, Le Populaire et L'Humanité. Mis ensemble, ces journaux représentent l'essentiel du panorama politique français. Les journaux de droite se firent de moins en moins critiques vis-à-vis de l'URSS, sans pour autant abandonner leur méfiance. Ceux de gauche soutinrent le rapprochement, tout en restant incrédules quant à la situation réelle. Cette recherche en est une de la perspective de l'autre, du rôle des médias dans la société et de l'influence de l'idéologie politique.

Les diplômés – no 338, mars/avril 1982

Pour toute demande de reproduction de contenu se trouvant dans cette publication, communiquer avec l’Association des diplômés de l’UdeM.

Les diplômés – no 278, mars/avril 1981

Pour toute demande de reproduction de contenu se trouvant dans cette publication, communiquer avec l’Association des diplômés de l’UdeM.