988 resultados para Montchrestien, Antoine de, ca. 1575-1621.


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Contient : Rome (1513-1658). — Pièces diverses, relatives aux affaires de Rome, 1513-1527 (f. 1) ; « Lettre du Roy au cardinal de Rambouillet, sur le sujet de la liberté du comte Gaiasse », 1571 ; « Commentarius caussarum belli a Paulo IIII, Pont. Max., in Italia suscepti anno 1556 », pièce anciennement paginée 509-528 ; Manifeste en faveur de Marc-Antoine Colonna, 1572 ; Minutes de lettres de Charles IX, à l'occasion de la maladie de Pie V, 1572 ; « Relatione dell'illustrissimo seignore Giovanni Dolfino, cavalliere e procuratore di Santo-Marco, ritornato d'ambasciatore à Roma l'anno 1598 » ; « Discours de l'Estat de l'Esglise et court de Rome », 1604, par J. Bosc ; Pièces relatives à divers conclaves ; Relations de la mort et éloges de Clément VIII (f. 173), — et du cardinal Baronius (f. 174) ; Pièces relatives à l'élection de Grégoire XV, 1621 ; « Relation des affaires de la cour de Rome..., faite par le sr de Brèves », 1623 ; Pièces relatives à l'élection d'Urbain VIII, 1623 ; Relation de la cour de Rome, 1624 ; Pièces relatives à l'élection d'Innocent X, 1644 ; « Mémoire, fait durant la maladie du pape Innocent X, des noms des cardinaux, de leurs aages et qualitez », 1655 ; Pièces relatives à l'élection d'Alexandre VII, 1655 ; « Relatione del clarissimo Mgr Bernardo Navagiero, che fu poi cardinale, ritornando da Roma ambasciatore à papa Paolo quarto, l'anno 1558 » ; « Il sussesso della morte di signori Carafi, con la declaratione et il modo che morirono » ; Mémoire sur la Cour pontificale au temps de Paul V, vers 1615 (f. 457) ; Venise (XVIe siècle-1627). — « Discours de l'évesque de Rodez [Georges d'Armagnac], ambassadeur pour le Roy à Venise... » (f. 291) ; « Mémoire pour... faire sçavoir les payemens ordonnez à la seigneurie de Venise et au duc de Florence, sur les prests par eux faicts au Roy », 1573 (f. 293), — et autres pièces concernant Venise et principalement les relations de Venise avec la France (f. 294) ; Pièces relatives aux différends entre les papes Clément VIII et Paul V et les Vénitiens, 1600-1607 ; « Relation de Venize, de l'année 1627 » ; Gênes (1575-1629). — « Relazione di Genova », 1575, mémoire très détaillé (f. 367) ; « Relatione della cità et dominio Genovese », 1580 ; Autre relation, adressée à Charles IX ; « Instruction baillée à Monsieur de Sabran, envoyé... vers le duc et la seigneurie de Gênes », 1629 (f. 440) ; Lucques . — « Mémoire de l'Estat de Lucques, depuis 1303 jusques en 1400... » (f. 446)

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Preliminary detrital zircon age distributions from Mazatzal crustal province quartzite and schist exposed in the Manzano Mountains and Pedernal Hills of central New Mexico are consistent with a mixture of detritus from Mazatzal age (ca. 1650 Ma), Yavapai age (ca. 1720 Ma.), and older sources. A quartzite sample from the Blue Springs Formation in the Manzano Mountains yielding 67 concordant grain analyses shows two dominant age peaks of 1737 Ma and 1791 Ma with a minimum peak age of 1652 Ma. Quartzite and micaceous quartzite samples from near Pedernal Peak give unimodal peak ages of ca. 1695 Ma and 1738 Ma with minimum detrital zircon ages of ca. 1625 Ma and 1680 Ma, respectively. A schist sample from the southern exposures of the Pedernal Hills area gives a unimodal peak age of 1680 Ma with a minimum age of ca. 1635 Ma. Minor amounts of older detritus (>1800 Ma) possibly reflect Trans-Hudson, Wyoming, Mojave Province, and older Archean sources and aid in locating potential source terrains for these detrital zircon. The Blue Springs Formation metarhyolite from near the top of the Proterozoic section in the Manzano Mountains yields 71 concordant grains that show a preliminary U-Pb zircon crystallization age of 1621 ¿ 5 Ma, which provides a minimum age constraint for deposition in the Manzano Mountains. Normalized probability plots from this study are similar to previously reported age distributions in the Burro and San Andres Mountains in southern New Mexico and suggest that Yavapai Province age detritus was deposited and intermingled with Mazatzal Province age detritus across much of the Mazatzal crustal province in New Mexico. This data shows that the tectonic evolution of southwestern Laurentia is associated with multiple orogenic events. Regional metamorphism and deformation in the area must postdate the Mazatzal Orogeny and ca. 1610 Ma ¿ 1620 Ma rhyolite crystallization and is attributed to the Mesoproterozoic ca. 1400 ¿ 1480 Ma Picuris Orogeny.

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Written in one column, 21 lines per page, in black and red.

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We present sea surface, upper thermocline, and benthic d18O data, as well as temperature and paleoproductivity proxy data, from the International Marine Global Change Study Program (IMAGES) Core MD06-3067 (6°31'N, 126°30'E, 1575 m water depth), located in the western equatorial Pacific Ocean within the flow path of the Mindanao Current. Our records reveal considerable glacial-interglacial and suborbital variability in the Mindanao Dome upwelling over the last 160 kyr. Dome activity generally intensified during glacial intervals resulting in cooler thermocline waters, whereas it substantially declined during interglacials, in particular in the early Holocene and early marine oxygen isotope stage (MIS) 5e, when upwelling waters did not reach the thermocline. During MIS 3 and MIS 2, enhanced surface productivity together with remarkably low SST and low upper ocean thermal contrast provide evidence for episodic glacial upwelling to the surface, whereas transient surface warming marks periodic collapses of the Mindanao Dome upwelling during Heinrich events. We attribute the high variability during MIS 3 and MIS 2 to changes in the El Niño Southern Oscillation state that affected boreal winter monsoonal winds and upper ocean circulation. Glacial upwelling intensified when a strong cyclonic gyre became established, whereas El Niño-like conditions during Heinrich events tended to suppress the cyclonic circulation, reducing Ekman transport. Thus, our findings demonstrate that variations in the Mindanao Dome upwelling are closely linked to the position and intensity of the tropical convection and also reflect far-field influences from the high latitudes.

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"The editor has reprinted the first edition of 1602, page for page, line for line, and with the original ornaments. Poems from the three later editions (1608, 1611, 1612 [i.e. 1621]) have been added."--Publisher's note.

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Mode of access: Internet.