Paul Warnefried's, Diakons von Forum-Julii Geschichte der Langobarden : zum erstenmale nach einem Codex der königlichen Bibliothek zu Bamberg aus dem Xten Jahrhundert /

Mode of access: Internet.

Panégyrique de Sainte Geneviève, patrone de Paris, prononcé dans son temple le jour de la fête du miracle des ardens.

Mode of access: Internet.

Johann Hasil von Nepomuk : Gedicht in zwei Abtheilungen /

Mode of access: Internet.

Cynewulfs Elene (Kreuzauffindung) : mit Einleitung, Glossar, Anmerkungen und der lateinischen Quelle /

Includes bibliographical references and index.

The register of Thomas de Cantilupe, Bishop of Hereford (A.D. 1275-1282) /

Includes index.

The ascetic life. The four centuries on charity.

Bibliography: p. 211-213.

Evtropi Breviarvm ab vrbe condita cvm versionibvs graecis et Pavli Landolfiqve additamentis.

Greek version by Paeanius.

Wives and mothers in the olden time : from French, Italian, and Latin authors /

Mode of access: Internet.

Swiety Jacek Odrowaz : jego zycie i czyny.

Mode of access: Internet.

Ars Donati quam Paulus Diaconus exposuit. Nunc primum ex Cod. vaticano-palatino 1746 monachi archicoenobii Montis Cassino in lucem proferunt.

Praefatio signed: Ambrosius Maria Amelli.

S. Maximi scholia in eos Dionysii libros quie extant. Michaelis Syngeli laudation eiusdem.

Vol. 3 of Dionysii Areopagitae opera quae extant ... 1561-62. cf. British Museum catalogue.

Magmatismo há ca. 660 - 640 Ma no Domínio Socorro: Registros de convergência-colisional na Aglutinação do Gondwana Ocidental

Uranium-lead zircon ages between 660 and 640 Ma, obtained from a series of calc-alkaline orthogneisses and plutons in southeast Brazil's Central Mantiqueira Province, suggest that a significant period of magmatism occurred in this region prior to the collisional assembly of West Gondwana (presently constrained in the region between ca. 625 and 580 Ma). While the nature of this earlier magmatism is presently unclear, some preliminary Sm-Nd data suggest that these magmas were not solely derived from the Paleoproterozoic lithosphere, but appear to represent hybrid products of Paleoproterozoic and Neoproterozoic sources. As such hybrid mixtures have been most commonly observed in continental are settings, it is possible that the 660 to 640 Ma magmatism represents are magmatism that resulted from subduction of Neoproterozoic oceanic crust during early precollisional convergence and closure of a branch of either the Adamastor or Goianides oceans.

Early Variscan I-type pluton in the pre-Alpine basement of the Western Alps: The ca. 360 Ma Cogne diorite (NW-Italy)

Located at the internal border of the Grand-Saint-Bernard Zone, the diorite and its aureole lie on top of intensively studied Alpine eclogitic units but this pluton, poorly studied yet, has kept locally almost undeformed. The pluton intruded, at similar to 360 Ma, country-rocks mostly composed of dark shales with Na2O > K2O and minor mafic intercalations of tholeiitic basalt affinity. This association is characteristic of the Vanoise (France) basement series, where available age determinations suggest an Early Paleozoic age. Parts of the pluton, and of its hornfels aureole that is evidenced here for the first time, in the Punta Bioula section of Valsavaranche valley (NW-Italy), have been well-preserved from the Alpine deformation. Syn-emplacement hardening, dehydration-induced, probably prevented strain-enhanced Alpine recrystallization. Magmatic rock-types range continuously from subordinate mafic types at SiO2 similar to 48%, of hornblendite with cumulative or appinite affinities, to the main body of quartz diorite to quartz monzonite (SiO2 up to 62%). P-T estimates for the pluton emplacement, based on the abundance of garnet in the hornfelses, using also zircon and apatite saturation thermometry and Al-in-hornblende barometry, suggest T similar to 800-950 degrees C and minimum P in the 0.2-0.5 GPa range, with records of higher pressure conditions (up to 1-2 GPa?) in hornblendite phlogopite-cored amphibole. The high-K, Na > K, calcalkaline geochemistry is in line with a destructive plate-margin setting. Based on major element data and radiogenic isotope signature (epsilon Nd-360 Ma from -1.2 to + 0.9, Sr-87/Sr-86(360 MA) from 0.7054 to 0.7063), the parental magmas are interpreted in terms of deep-seated metabasaltic partial melts with limited contamination from shallower sources, the low radiogenic Nd-content excluding a major contribution from Vanoise tholeiites. There is no other preserved evidence for Variscan magmatism of similar age and composition in the Western Alps, but probable analogs are known in the western and northern parts of French Massif Central. Regarding the Alpine tectonics, not only the age of the pluton and its host-rocks (instead of the Permo-Carboniferous age previously believed), but also its upper mylonitic contact, suggest revisions of the Alpine nappe model. The Cogne diorite allegedly constituted the axial part of the E-verging ``pli en retour [backfold] du Valsavaranche'', a cornerstone of popular Alpine structural models: in fact, the alleged fold limbs, as attested here by field and geochemical data, do not belong to the same unit, and the backfold hypothesis is unfounded. (C) 2012 Elsevier B.V. All rights reserved.