105 resultados para Missale Gothicum.
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Trägerband: Inc. qu. 1011
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Trägerband: Ms. lat. oct. 27; Vorbesitzer: Johann Hartmann Beyer
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Trägerband: Ms. lat. oct. 24; Ms. lat. oct. 25; Vorbesitzer: Johann Hartmann Beyer
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Trägerband: Ausst. 121; Vorbesitzer: Konrad Bender (Doliatoris); Bartholomaeusstift Frankfurt am Main
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Trägerband: Biblioth. Ff. Stadtbibl. 560; Vorbesitzer: Johann Hartmann Beyer
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Trägerband: Inc. oct. 414; Vorbesitzer: Karmeliterkloster Frankfurt am Main
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Acquis le 21 septembre 1860 de M. Magniat, 10 rue des Saussaies, pour le prix de 600 francs; cf. B.n.F., département des Manuscrits, registre des acquisitions 1848-1893, n° 5464 "Psalterium davidicum et missale vetus, in 4° vél. Ms. du XIIe s."; signalé par Delisle dans les acquisitions de 1860, cf. Cab. des mss., II, 306. Note : « ce psautier a été à l'usage d'une Eglise d'Angleterre, et a été apporté au diocèse de Sens au XIV siécle, auquel tems un moine du mesme diocèse de Sens y a ajouté plusieurs SS. De pays dans les six derniers mois » (2).
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Missale Romanvm auctoritate Pavli V Pont. M. Sinice redditum a P. Lvdovico Bvglio soc. Iesv Pekini In Collegio ejusd. Soc. An. MDCLXX.Titre Chinois en rouge, au verso nom du traducteur et autorisation du P. Verbiest ; frontispice avec titre latin en rouge et noir. Papier à encadrements rouges pour la table, noir pour le texte ; notes en rouge.
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Esta dissertação analisa a conexão existente entre o mercado de dívida pública e a política monetária no Brasil. Com base em um Vetor Auto-Regressivo (VAR), foram utilizadas duas proxies alternativas de risco inflacionário para mostrar que choques positivos no risco inflacionário elevam tanto as expectativas de inflação do mercado quanto os juros futuros do Swap Pré x DI. Em seguida, com base em modelo de inconsistência dinâmica de Blanchard e Missale (1994) e utilizando a metodologia de Johansen, constatou-se que um aumento nos juros futuros diminui a maturidade da dívida pública, no longo prazo. Os resultados levam a duas conclusões: o risco inflacionário 1) dificulta a colocação de títulos nominais (não-indexados) no mercado pelo governo, gerando um perfil de dívida menos longo do que o ideal e 2) torna a política monetária mais custosa.
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Esta dissertação analisa a conexão existente entre o mercado de dívida pública e a política monetária no Brasil. Com base em um Vetor Auto-Regressivo (VAR), foram utilizadas duas proxies alternativas de risco inflacionário para mostrar que choques positivos no risco inflacionário elevam tanto as expectativas de inflação do mercado quanto os juros futuros do Swap Pré x DI. Em seguida, com base em modelo de inconsistência dinâmica de Blanchard e Missale (1994) e utilizando a metodologia de Johansen, constatou-se que um aumento nos juros futuros diminui a maturidade da dívida pública, no longo prazo. Os resultados levam a duas conclusões: o risco inflacionário 1) dificulta a colocação de títulos nominais (não-indexados) no mercado pelo governo, gerando um perfil de dívida menos longo do que o ideal e 2) torna a política monetária mais custosa.
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Vorbesitzer: Dominikanerkloster Frankfurt am Main;
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Five of the six sites drilled during Leg 77 of the Deep Sea Drilling Project yielded Cretaceous sediments. Two of these sites, 535 and 540, form a composite section that spans the upper Berriasian through most of the Cenomanian. Olive black marly limestones in this interval yield relatively rich, well-preserved nannofossil assemblages that allow biostratigraphic subdivision of the sequence. This composite section provides important information on the Early Cretaceous history of the Gulf of Mexico, as well as additional information on tropical Lower Cretaceous nannofossil assemblages. The post-Cenomanian nannofossil (and sedimentary) record is limited to a thin, condensed section of Santonian through lower Maestrichtian pelagic sediments at one site (538) and is absent or represented by redeposited material at the other sites. Two new genera, Perchnielsenella and Darwinilithus, are described. Two new taxa, Darwinilithus pentarhethum and Lithraphidites acutum ssp. eccentricum, are described; and two new combinations, Rhagodiscus reightonensis and Perchnielsenella stradneri, are propose.
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Two of five holes drilled at two separate sites during Leg 123 of the Ocean Drilling Program intersected thick and relatively complete sections of Upper Cretaceous-Paleogene nannofossiliferous sediments. Although dominated by turbidite deposition in the upper part, Hole 765C contains a thick and relatively complete Albian-Oligocene section, including a particularly thick Aptian interval, with abundant and fairly well-preserved nannofossils. Several unconformities are confidently interpreted in this section that span much of the Santonian, late Campanian, Maestrichtian, late Eocene, and early Oligocene. Hole 766A contains a thick and relatively complete Albian-lower Eocene section having generally abundant and well-preserved nannofossils. Several unconformities also have been identified in this section that span much of the Coniacian, early Campanian, Maestrichtian, and late Eocene through early Pliocene. The chronostratigraphic position and length of all these unconformities may have considerable significance for reconstructing the sedimentary history and for interpreting the paleoceanography of this region. A particularly thick section of upper Paleocene-lower Eocene sediments, including a complete record across the Paleocene/Eocene boundary, also was cored in Hole 766A that contains abundant and diverse nannofossil assemblages. Although assemblages from this section were correlated successfully using a standard low-latitude zonation, difficulties were encountered that reduced biostratigraphic resolution. Several lines of evidence suggest a mid-latitude position for Site 766 during this time, including (1) high assemblage diversity characteristic of mid-latitude zones of upwelling and (2) absence of certain ecologically controlled markers found only in low latitudes.
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Ocean Drilling Program (ODP) Leg 210 is one of very few deep-sea legs drilled along the eastern Canadian continental margin. Most other drilling on this margin has been carried out by the petroleum industry on the shallow-water regions of the Scotian shelf and the Grand Banks (see Doeven, 1983, for nannofossil studies). Deep Sea Drilling Project (DSDP) Leg 12 Site 111 and ODP Leg 105 Site 647 were drilled in the general vicinity of Leg 210 but recovered no appreciable Lower Cretaceous (Albian-Cenomanian) sediments. Site 111 yielded indurated limestones dated tentatively as late Albian-early Cenomanian, whereas Site 647 encountered no Albian-Cenomanian sediments. Two sites (Sites 1276 and 1277) were drilled during Leg 210 in the Newfoundland Basin with the primary objective of recovering basement rocks to elucidate the rifting history of the North Atlantic Basin. The location for Leg 210 was selected because it is conjugate to the Iberia margin, which was drilled extensively during DSDP/ODP Legs 47B, 103, 149, and 173. A secondary but equally important objective was to recover the overlying sediments with the purpose of studying the postrift sedimentation history of this margin.