325,230 research outputs found
L' Homme Aux Quarante Écus / [Voltaire]
No full textKenntnisse zur Veröffentlichungsangabe 2020 korrigiert, 2011, zum Zeitpunkt der Bearbeitung für das VD18, wurde Genf als Erscheinungsort angenommenVerf. bei Barbier ermitteltGenfer Ausgabe cf. BLC, Nr. 001723867 abweichendSignaturformel: pi2 A-G8 H4 [$ 4(-H3,4) bezeichnet, römische Ziffern: ij, iij, iiij; F3 bezeichnet als 'P iij']Kustoden am Ende der Lagen und auf den Seiten 4, 40, 63, 98, 114, 115 und 118; separate Kustoden für Fußnoten (vgl. S. 114). – Ohne PaginierfehlerAnführungszeichen zu Beginn der Zitate und am linken Textrand in Form von Doppelkommata, am Ende der Zitate als schließendes Gegenstück ein kopfstehender Doppelapostroph (vgl. S. 83-86)Vorlageform des Erscheinungsvermerks: 1768. - Laut bibliographischem Nachweis in der Werkausgabe OCV mutmaßlich bei Lacombe in Paris erschiene
Título: La médecine rappallée á sa premiere simplicité
No full textCopia digital : Google booksSign.: a\p12\s, A-O\p12\s, P\p5\s ; A-Q\p12\s, R\p10\sError en sign. tipográficas t. II: en A5, pone A6, en R5, y R6, pone C5 y C6 respectivamenteCabecera con viñeta adorno xi
Dictionnaire raisonné de diplomatique ...
No full textSign. : a\p8\s, b\p4\s, A-Z\p8\s, 2A-2L\p8\s, 2M\p2\sAnte
Título: La destruction de l'empire du Pérou
No full textSign.: a\p8\s, b\p4\s, C-X\p8\sP. 327 numerada erróneamente como p. 329Error de pag., de p. 168 pasa a 171Las h. de grab. calc., intercaladas en el text
Dictionnaire Classique de Geographie Ancienne ... servant d'introduction a celui de la Geographie Moderne de Laurent Echard.
No full textSign.: a\p8\s, b\p2\s, b\p4-7\s, []\p2\s, A-2Q\p8\s, 2R\p4\sTexto a dos colSign.: a\p8\s, b\p2\s, b\p4-7\s, [ ]\p2\s, A-Z\p8\s, 2A-2Q\p8\s, 2R\p4\sIlustraciones xi
Dictionnaire du citoyen : ou abrégé historique : théorique et pratique du commerce ... : tome premier.
No full textSegún "Bibliographie Française" o autor é Honoré Lacombe de PrezelSign.: a\p8\s, b\p4\s, A-2D\p8\s, 2E\p5\sTexto a dos colAntepSign.: a, b, A-Z, 2A-2D, 2ETexto a dúas colContiene: A-G
Mechanical constraints on the development of the Zagros Folded Belt (Fars)
No full textWe synthesize available structural, seismotectonics and microtectonics studies, mechanical modelling of the topography as well as stratigraphic constraints on the timing of Plio-Pleistocene folding and Zagros basin evolution in order to examine which mechanical behaviour would explain the development of the Zagros Folded Belt at both local and regional scale. At the local scale we focus on the mechanism of cover folding and internal deformation of cover rocks. At the regional scale we focus on crustal rheology that led to the observed regional topography. Recent mechanical constraints derived from a critical wedge modelling of the regional topography together with available structural studies and seismotectonic studies confirm that the basement is necessarily involved in the deformation. Additionally, crustal rheology should involve a sufficiently strong lower crust to maintain the topography. Stratigraphic data on the basin scale suggests that the deformation in the Zagros Folded Belt initiated by inversion of the inherited N-S and NW-SE-trending marginal structures in the early Miocene. At 5-3 Ma, the intraplate stresses have increased sufficiently in response to ongoing convergence to exceed the brittle strength of the pre-fractured basement and then to produce the initiation of the Zagros uplift. This event occurred simultaneously with the rapid development of cover folding until the Bakhtyari conglomerates were deposited unconformably on these structures as the fold growth decreased. The Hormuz salts at the base of the pile allowed the upper sedimentary cover to be decoupled from the basement but there is no evidence of independent development through time. This is confirmed by the kinematical consistency of the Mio-Pliocene small-scale faulting in the cover and seismogenic faulting reflecting the internal deformation of basement and cover, despite the occurrence of the thick Hormuz salt layer. Buckling of the cover rocks, rather than thinskinned propagation of the Zagros Folded Belt, is proposed to be a more reliable mechanism to account for stratigraphic data, field observations, structural studies, microtectonic data and mechanical modelling. We finally conclude that the overall thick-skinned deformation that followed the initial margin inversion was probably coeval with cover folding (buckling). The way basement and cover deform is thus remarkably different; the basement is pre-fractured so it shortens preferentially by faulting. In contrast, the folding (buckling) of the sedimentary cover developed with the assistance of plastic-viscous processes.F. Mouthereau, O. Lacombe, J. Tensi, N. Bellahsen, S. Kargar, K. Amrouc
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