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Relevant bibliographies by topics / Place des Vosges

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Academic literature on the topic 'Place des Vosges'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 March 2023

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Journal articles on the topic "Place des Vosges"

1

Hoft-March, Eilene. "Place des Vosges par Michel Braudeau." French Review 91, no. 2 (2017): 247. http://dx.doi.org/10.1353/tfr.2017.0023.

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2

Sanson, Luc. "Grand (Vosges). Place de la Fontaine et place des Halles." Archéologie médiévale, no. 51 (December 20, 2021): 186. http://dx.doi.org/10.4000/archeomed.41420.

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Dohr, Myriam. "Épinal (Vosges). Place de l’Âtre, rue Jeanmaire, rue de la Maix." Archéologie médiévale, no. 46 (December 1, 2016): 256–57. http://dx.doi.org/10.4000/archeomed.7406.

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Faure, Michel, Eugène Be Mezeme, Alain Cocherie, Jérémie Melleton, and Philippe Rossi. "The South Millevaches Middle Carboniferous crustal melting and its place in the French Variscan belt." Bulletin de la Société Géologique de France 180, no. 6 (October 1, 2009): 473–81. http://dx.doi.org/10.2113/gssgfbull.180.6.473.

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AbstractSeveral episodes of crustal melting are now well identified in the Variscan French Massif Central. Middle Devonian (ca 385-375 Ma) migmatites are recognized in the Upper and Lower Gneiss Units involved in the stack of nappes. Late Carboniferous migmatites (ca 300 Ma) are exposed in the Velay Massif only and Middle Carboniferous migmatites crop out in the Para-autochthonous Unit and southern Fold-and-Thrust Belt. In the SW part of the Massif Central, the South Millevaches massif exposes migmatites developed at the expense of ortho- and paragneiss. They form kilometer-sized septa within the foliated Goulles leucogranitic pluton, which is in turn intruded by the non-foliated Glény two micas granite pluton. Monazite grains extracted from these three rock-types have been dated by the EPMA chemical method. Three samples of migmatite yield a late Visean age (ca 337-328 Ma), the Goulles and Glény granitic plutons yield ages at 324-323 Ma and 324-318 Ma, respectively. These new results enlarge the evidence of a Middle Carboniferous crustal melting imprint that up to now was only reported in the eastern part of the French Massif Central, in the northern Cévennes and in the Montagne Noire axial zone. At the scale of the French Variscan massifs, the Visean crustal melting event is conspicuously developed since it is recognized from the Massif Armoricain (Vendée and south coast of Brittany) to the Central Vosges. This episode is synchronous with the huge thermal event responsible for the “Tuffs anthracifères” magmatism of the northern Massif Central and Vosges, and took place immediately after the last thickening phase recorded both in Montagne Noire and Ardennes, that is on the southern and northern outer zones of the Variscan Belt, respectively. However, the geodynamic significance of this major event is not fully understood yet.

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Thirion, Erwin. "Les chênes remarquables de la tranchée du chêne des partisans de Saint-Ouen-les-Parey (Vosges)." Revue forestière française 73, no. 1 (December 7, 2021): 67–77. http://dx.doi.org/10.20870/revforfr.2021.4935.

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La mise en place du quart de réserve des forêts à partir de l’Ordonnance de 1669 a permis la production d’arbres aux dimensions majestueuses dans toutes les forêts de France. Dans le département des Vosges, le quart de réserve de la commune de Saint-Ouen-lès-Parey a connu l’existence de cinq chênes majestueux, dont un seul subsiste aujourd’hui. Cette synthèse bibliographique a pour objectif de proposer une description dendrométrique et historique de ces chênes plusieurs fois centenaires.

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Bourlange, Sylvain, Mahmoud Mekkawi, Marianne Conin, and Pierre-André Schnegg. "Magnetotelluric study of the Remiremont-Epinal-Rambervillers zone of migrating seismicity, Vosges (France)." Bulletin de la Société Géologique de France 183, no. 5 (September 1, 2012): 461–70. http://dx.doi.org/10.2113/gssgfbull.183.5.461.

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AbstractThe magnetotelluric method has been used to image the deep electrical structure of the Remiremont-Epinal-Rambervillers region in the French Vosges Massif, which has presented a significant seismic activity in the past decades. Several earthquakes of moderate magnitude (up to 5.1) occurred in this area with a systematic migration along a nearly N-S direction. Inversion of the magnetotelluric data reveals zones of high electrical conductivity. A large conductive body presents a significative spatial correlation with the region that was most recently affected by earthquakes. This conductive body is interpreted as a consequence of the presence of a fluid filled basement fault network in proximity to the zone affected by the last seismic crisis, where fluid pressure diffusion takes place for several years after the main shock and participates in maintaining a microseismic activity.

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Schwartz, Dominique, Vincent Robin, Pierre Adam, Philippe Schaeffer, Anne Gebhardt, Pierre-Alexis Herrault, Benjamin Keller, et al. "Les géosciences au service de l’archéologie agraire. Une étude de cas sur les rideaux de culture de Goldbach (68)." Archimède. Archéologie et histoire ancienne 7 (June 9, 2020): 205–16. http://dx.doi.org/10.47245/archimede.0007.act.08.

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Les rideaux de culture sont des talus qui se forment involontairement à l’amont d’une haie, par accumulation de colluvions érodés dans les champs. Ils peuvent constituer des parcellaires de très grande extension spatiale, caractérisés par des parcelles étroites, allongées perpendiculairement à la pente. L’histoire de ces parcellaires et leur datation sont encore très mal connues. Les résultats présentés ici concernent un parcellaire de plusieurs centaines d’hectares localisé à Goldbach-Altenbach, dans les Vosges haut-rhinoises. Les résultats obtenus sur deux coupes transversales à des rideaux de culture montrent que le parcellaire a été mis en place vers 900 AD, puis que la zone a été brièvement abandonnée pendant la Guerre de Trente Ans. La datation vers 900 AD suggère que ce parcellaire a été mis en place sous l’autorité de l’abbaye de Murbach. L’ensemble de la zone a en effet été donné à cette abbaye vers 800 AD.

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8

Derntl, Maria Fernanda. "O início da história de duas praças do século 17: a Place des Vosges, em Paris, e Covent Garden, em Londres." Pós. Revista do Programa de Pós-Graduação em Arquitetura e Urbanismo da FAUUSP, no. 20 (December 1, 2006): 140. http://dx.doi.org/10.11606/issn.2317-2762.v0i20p140-157.

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Bourgeois, David. "Le marchand bâlois, ses mines et ses réseaux ou l’émergence du capitalisme rhénan au xve siècle." Cinquante ans de désindustrialisation, no. 1 (January 1, 2019): 175–93. http://dx.doi.org/10.57086/rrs.92.

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L’extraction de l’argent dans l’Occident médiéval, activité en constant essor tout au long de ce millénaire, donne lieu à l’ouverture de nombreux filons sur l’ensemble du territoire européen. Dans l’aire du Rhin supérieur, bordée par les massifs des Vosges et de la Forêt-Noire, la production argentifère s’avère particulièrement dynamique. En Haute-Alsace et dans le Brisgau, au xve siècle, l’extraction de l’argent se trouve dopée par des capitaux urbains, en grande partie bâlois. L’étude des marchands bâlois et de leurs activités minières laisse apparaître les contours d’une société où se concentrent pouvoirs économique, politique et culturel et dans laquelle le système familial occupe une place centrale. Les domaines diversifiés dans lesquels interviennent ces marchands, dont celui, essentiel, de l’extraction minière mettent en évidence le fort potentiel économique de ces familles et l’émergence d’un capitalisme rhénan qui va se développer au cours des siècles suivants.

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Cope, J. C. W., P. D. Guion, G. D. Sevastopulo, and A. R. H. Swan. "Carboniferous." Geological Society, London, Memoirs 13, no. 1 (1992): 67–86. http://dx.doi.org/10.1144/gsl.mem.1992.013.01.9.

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AbstractCarboniferous geology has developed very rapidly over the past two decades since ideas on sedimentology and new radiometric scales, together with new biostratigraphical schemes based on miospores, conodonts and foraminifera have been synthesized with ideas on plate tectonic processes, climatic changes and oscillations of sea level. The application of the McKenzie model of basin development to the Carboniferous, and the relating of eustatic sea-level changes, which had a profound effect on Carboniferous palaeo-geography, to fluctuations in the size of the Gondwanan ice sheets, have been major factors in the understanding of Carboniferous processes. The Carboniferous evolution of Britain took place to the (present) north of a plate suturing occurring along a line extending from Galicia, through Armorica and the Massif Central to the Vosges, during mid Devonian to early Carboniferous times. In front of this collision zone was the Rheno-Hercynian zone which opened probably during mid Devonian times and which was partly floored by oceanic crust; its closure can be traced through to late Carboniferous times as a series of northwardly directed thrust complexes. To the (present) north of this zone was a foreland on which basins developed on either side of a persistent Wales-London-Brabant High. Studies by Dewey (1982) and Leeder (1982, 1987, 1988) have shown that late Devonian to early Carboniferous extension, involving β factors of up to 2, produced a series of grabens and half-grabens in the Caledonian basement. These developing structures were the dominant control on early Carboniferous sedimentation and produced a sea-bed topography which was

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Dissertations / Theses on the topic "Place des Vosges"

1

Muller, Yves. "L'Avifaune forestière nicheuse des Vosges du Nord : sa place dans le contexte médio-européen." Dijon, 1985. http://www.theses.fr/1985DIJOS029.

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Lakhrissi, Moulay Abdessamad. "Pétrologie, minéralogie, géochimie du volcanisme dévono-dinantien des Vosges méridionales (France) : sa place dans le contexte géodynamique varisque." Lille 1, 1996. https://pepite-depot.univ-lille.fr/LIBRE/Th_Num/1996/50376-1996-168.pdf.

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Les formations volcaniques dévono-dinantiennes des Vosges méridionales ont été regroupées en trois unités lithostratigraphiques successives : unité I – unité II – unité III. Les études pétrographiques, minéralogiques (cristallochimie des clinopyroxènes reliques), géochimiques (majeurs – traces) attribuent un caractère orogènique à l’ensemble de ce volcanisme. Les termes basiques de l’unité I sont à caractère tholéiitique d’arc, certains présentant un caractère calco-alcalin. L’unité II est calco-alcaline. L’unité III possède des affinités shoshonitiques. Les données géochimiques suggèrent que ces magmas sont issus d’une même source mantellique appauvrie ayant acquis, par différents mécanismes d’enrichissement, des caractères géochimiques caractéristiques de manteau de zone de substitution. La participation crustale dans la genèse de ce magmatisme croît des laves de l’unité I à celles de l’unité III. La place de ce volcanisme dans le cadre géodynamique varisque mérite réflexion. La signature orogénique des laves et leur typologie successive sont compatibles avec une mise en place dans un contexte de marge active et de zone de subduction. Les modèles géodynamiques d’évolution de la chaîne varisque montrent des divergences à propos de l’existence d’aires océaniques actives au carbonifère. Pour expliquer l’évolution du magmatisme, un modèle associant subduction, puis collision, peut être proposé.

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3

Dahire, Mohamed. "Granites et leucogranites péralumineux du Brezouard et du Bilstein (Vosges moyennes) : caractères pétrographiques, géochimiques et minéralogiques." Nancy 1, 1988. http://www.theses.fr/1988NAN10027.

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L'étude des leucogranites péralumineux des Massifs de Brezouard et de Bilstein (Vosges moyennes) a pour objectif une cartographie détaillée, une caractérisation pétrographique, minéralogique et géochimique des différents faciès (leucogranite A 2 micas, leucogranite à cordiérité, filon microgranitique, rhyolite à cordiérité) et de définir les modalités d'évolution ainsi que leurs relations spatiales et génétiques. Pour le massif de Brezouard, une mise en place biphasée avec une déformation périphérique en partie subsynchrone oblitérée ultérieurement par une autre cataclastique de basse température est mise en évidence. Le massif de Bilstein correspond à une structure indépendante et aurait subi une orthognéissification en relation avec le fonctionnement ductile d'une zone de cisaillement destre

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4

Leon, Carol. "Movement and belonging : lines, places and spaces of travel in selected writings of Naipaul, Ondaatje, Lawrence and White." Phd thesis, 2000. http://hdl.handle.net/1885/147337.

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Books on the topic "Place des Vosges"

1

Siguret, Catherine. Le mouton de la place des Vosges: Roman. Paris: Albin Michel, 2015.

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2

Feist, Raymond E. Koning der vossen. Amsterdam: Uitgeverij M, 2004.

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3

Blohm & Voss 155. Sturbridge, Massachusetts, USA: Monogram Aviation Publications, 1990.

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J, Nowarra Heinz. Blohm & Voss, Bv 222 Wiking, Bv 238. Atglen, PA: Schiffer Pub., 1997.

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5

Place des Vosges. SEUIL, 2017.

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6

Braudeau, Michel. Place des Vosges. SEUIL, 2017.

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7

Mazeran, Alain. Place des Vosges. Imprimerie nationale, 2002.

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Braudeau, Michel. Place des Vosges. SEUIL, 2017.

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9

Simenon, Georges. Sombras Na Place Des Vosges. Companhia das Letras2, 2015.

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10

Lacouture, Daniel. Inconnu de la Place des Vosges. Lulu Press, Inc., 2016.

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Book chapters on the topic "Place des Vosges"

1

Garrec, J. P., and M. Berteigne. "Recherches sur les Causes du Deperissement des Forets. Mise en Place de Tests D’Exclusion au Col du Donon (Vosges - France)." In Air Pollution and Ecosystems, 701–3. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-4003-1_83.

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Etlicher, Bernard. "French and Belgian Uplands." In The Physical Geography of Western Europe. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199277759.003.0022.

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The French Uplands were built by the Hercynian orogenesis. The French Massif Central occupies one-sixth of the area of France and shows various landscapes. It is the highest upland, 1,886 m at the Sancy, and the most complex. The Vosges massif is a small massif, quite similar to the Schwarzwald in Germany, from which it is separated by the Rhine Rift Valley. Near the border of France, Belgium, and Germany, the Ardennes upland has a very moderate elevation. The largest part of this massif lies in Belgium. Though Brittany is partly made up of igneous and metamorphic rocks, it cannot be truly considered as an upland; in the main parts of Brittany, altitudes are lower than in the Parisian basin. Similarities of the landscape in the French and Belgian Uplands derive from two major events: the Oligocene rifting event and the Alpine tectonic phase. The Vosges and the Massif Central are located on the collision zone of the Variscan orogen. In contrast, the Ardennes is in a marginal position where primary sediments cover the igneous basement. Four main periods are defined during the Hercynian orogenesis (Bard et al. 1980; Autran 1984; Ledru et al. 1989; Faure et al. 1997). The early Variscan period corresponds to a subduction of oceanic and continental crust and a highpressure metamorphism (450–400 Ma) The medio- Variscan period corresponds to a continent–continent collision of the chain (400–340 Ma). Metamorphism under middle pressure conditions took place and controlled the formation of many granite plutons: e.g. red granites (granites rouges), porphyroid granite, and granodiorite incorporated in a metamorphic complex basement of various rocks. The neo-Variscan period (340–320 Ma) is characterized by a strong folding event: transcurrent shear zones affected the units of the previous periods and the first sedimentary basins appeared. At the end of this period, late-Variscan (330–280 Ma), autochthonous granites crystallized under low-pressure conditions related to a post-collision thinning of the crust. Velay and Montagne Noire granites are the main massifs generated by this event. Sediment deposition in tectonic basins during Carboniferous and Permian times occurred in the Massif Central and the Vosges: facies are sandstone (Vosges), shale, coal, and sandstone in several Stephanian basins of the Massif Central, with red shale and clay ‘Rougier’ in the south-western part of the Massif Central.

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Roberts, Michelle Voss. "Introduction: A Place for Comparative Theology in Christian Systematic Reflection." In Comparing Faithfully. Fordham University Press, 2016. http://dx.doi.org/10.5422/fordham/9780823274666.003.0001.

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The editor, Michelle Voss Roberts, introduces the history and methods of comparative theology and argues for its importance in the study of systematics. The essays in the volume represent the best practices of comparative theology, exciting new approaches to it, and fresh perspectives on familiar topics in Christian systematic theology. The introduction suggests four uses for the volume: 1) as a way into Christian systematic theology; 2) as a way to test theological categories; 3) as proposals for doctrinal reflection; and 4) as an invitation to the reader to take up the activity of comparative reading.

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Winterbottom, Michael. "The Manuscript Tradition of [Quintilian]’s Major Declamations: A New Approach." In Papers on Quintilian and Ancient Declamation, edited by Antonio Stramaglia, Francesca Romana Nocchi, and Giuseppe Russo, 295–310. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780198836056.003.0024.

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This previously unpublished paper seeks to demonstrate that two twelfth-century manuscripts of the Major Declamations, Montpellier 226 and Paris, lat. 1618, are not, as had hitherto been supposed, independent primary witnesses to the text, but descend from an earlier extant manuscript, Bamberg, Class. 44. This manuscript has gaps at certain points where the rubricator did not complete his task; in these places the Montpellier and Paris manuscripts show either lacunae or words that can be argued to be late confections. The paper goes on to suggest, more tentatively, that the second branch of the tradition, here called Φ‎, is only superior to the lost parent of the Bambergensis and Leiden, Voss. lat. Q. 111 because its own lost ancestor had been subject to medieval conjecture. The paper ends by providing a sample of the kind of simplified apparatus criticus that could be constructed if this new approach is accepted.

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