88,079 research outputs found
Alien Registration- Rossignol, Joseph F. (Milford, Penobscot County)
No full texthttps://digitalmaine.com/alien_docs/8039/thumbnail.jp
La Feria de Sorotchintzi ; Le Rossignol
No full textDe cada obra s'ha digitalitzat un programa sencer. De la resta s'han digitalitzat les parts que són diferents.Empresa José F. ArquerEmpresa: Juan Mestres CalvetLa Feria de Sorotchintzi : Òpera de Modest Petrovitx Musorgski; Le Rossignol : òpera d'Igor Stravinsky i llibret d'Igor Stravinsky i Stepan Mitousoff, segons Hans Christian AndersenOrquestra Simfònica del Gran Teatre del Lice
Trois mélanoblastomes de siège inaccoutumé chez les bovidés
No full textLombard Charles, Puget E., Rogé F., Rossignol A. Trois mélanoblastomes de siège inaccoutumé chez les bovidés. In: Bulletin de l'Académie Vétérinaire de France tome 116 n°4, 1963. pp. 171-174
Geodynamic evolution of the Minas Basin, southern São Francisco Craton (Brazil), during the early Paleoproterozoic: Climate or tectonic?
No full textLike many other cratons around the world, the São Francisco Craton is characterized by an early Paleoproterozoic (2.5–2.1 Ga) unconformity that is reported worldwide as the result of global glacial events leading to a major sea-level drop. To document the duration and the cause(s) of the stratigraphic hiatus in the São Francisco Craton, this study provides U–Pb dates obtained on detrital zircon grains from the Piracicaba Group, which directly overlies the unconformity. Our results show that this sedimentary unit is younger than 2333 ± 11 Ma and consequently deposited during the late Siderian or the early Rhaycian. This maximum depositional age demonstrates that the early Paleoproterozoic stratigraphic gap lasted for at least 60 Ma. Based on quantitative analyses of the age distribution of the Piracicaba Group, we evidence a major shift in sedimentary provenance between the sedimentary units located below and above the unconformity. This change is interpreted to be directly related to the development of a subduction system along the southern and eastern margins of the São Francisco proto-craton. Our results indicate that regional geodynamic events, and not only global glacial events and their consequences, must be accounted for in Earth system models for the early Paleoproterozoic
The effects of short-term sprint training on MCT expression in moderately endurance-trained runners
No full textDale C. Bickham, David J. Bentley, Peter F. Le Rossignol, David Cameron-Smit
Le rossignol de Colombine : chanson vocalise [illustration Léon Pousthomis]
No full textLe rossignol de Colombine : chanson vocalise ; (dédicace) “Hommage à Me Cécile Laviolette et Me Dargenson” ; illustration Léon Pousthomis ; paroles de L. Kahm [L. Kahm (18..-19.. parolier non-identifié] et L. Colonge ; musique de Félix Michel et F. Galifer [Francis Galifer] ; Lyon-Chansons, Orgeret éditeur, 72 passage de l’Argue, Lyon ; imprimerie E. Dupré, Paris [intérieur : sans dédicace, sans date, cotage JMO636] ; verso vierge ; incipit “Dans le jardin de Colombine”. Datation 1912 (par dépôt légal BNF)
Le rossignol de Colombine : chanson vocalise [illustration Léon Pousthomis]
No full textLe rossignol de Colombine : chanson vocalise ; (dédicace) “Hommage à Me Cécile Laviolette et Me Dargenson” ; illustration Léon Pousthomis ; paroles de L. Kahn et L. Colonge ;musique de Félix Michel et F. Galifer ; Lyon-Chansons, Orgeret éditeur, 72 passage de l’Argue, Lyon ; imprimerie E. Dupré, Paris [intérieur : sans dédicace, sans date, cotage JMO636] ; verso vierge ; incipit “Dans le jardin de Colombine”. Datation 1912 (par dépôt légal BNF)
The International Study of Insulin and Cancer
No full textThe international study of insulin and cancer.
Grimaldi-Bensouda L, Marty M, Pollak M, Cameron D, Riddle M, Charbonnel B, Barnett AH, Boffetta P, Boivin JF, Evans M, Rossignol M, Benichou J, Abenhaim L; ISICA group
Le rossignol de Colombine : chanson vocalise [illustration Léon Pousthomis]
No full textLe rossignol de Colombine : chanson vocalise ; (dédicace) “Hommage à Me Cécile Laviolette et Me Dargenson” ; illustration Léon Pousthomis ; paroles de L. Kahm [L. Kahm (18..-19.. parolier non-identifié] et L. Colonge ; musique de Félix Michel et F. Galifer [Francis Galifer] ; Lyon-Chansons, Orgeret éditeur, 72 passage de l’Argue, Lyon ; imprimerie E. Dupré, Paris [intérieur : sans dédicace, sans date, cotage JMO636] ; verso vierge ; incipit “Dans le jardin de Colombine”. Datation 1912 (par dépôt légal BNF)
Post-collisional tectono-magmatic evolution, crustal fertilization, and ore genesis: the late Variscan metallogenic stages in Sardinia
No full textThe Variscan post-collisional tectonic and magmatic events were critical for ore deposits in the Paleozoic
massifs of Europe. In Sardinia, two main types of Variscan ore deposits can be recognized: (1) “orogenic”,
structurally-controlled deposits associated with shear zones and extensional structures; (2) granite intrusion
hosted/related deposits. Both types are unevenly distributed in the Paleozoic basement and in the Sardinian
batholith, being much more abundant in Southern Sardinia. “Orogenic” deposits include As-Au±Sb ± W and
Zn-Cu-Pb-Ag vein systems hosted in greenschist facies metamorphics. They result from multiple mineralization
stages from fluids of mixed (but dominantly metamorphic) origin at different structural levels in the nappe
stack of the Variscan front, during the post-collisional extension. Large-scale antiformal structures were traps
for fluids; base metal and As-Au-rich deposits prevail in deeper structural zones, whereas Sb-W (Au) deposits
are related with shallower extensional structures.
Granite-hosted/related deposits consist of Mo ± Cu greisens, Pb-Zn-Cu-Fe±Sn± W±Bi±F and Pb-Zn-Cu-
Fe±REE skarns, and W-Sn-Mo-Bi (±Te±Au) and Pb-Zn-F-Ba veins, also associated in magmatic-hydrothermal
systems. Most intrusion-hosted/related ores may be bracketed into the latest and narrow (290-285) Ma growth
stages of Sardinian Batholith. They are more abundant in southern Sardinia, associated to multiple suites of
F-rich granites, including a suite of Sn-W-Mo (Bi, In)-bearing, “rare metals” granites belonging to an ilmenite
rock-series (Naitza et al., 2017).
As evidenced in recent literature (Cocco et al., 2018; Secchi et al., 2022), the Paleozoic basement of
Sardinia is made of micro-terranes assembled by large-scale shear zones in the post-collisional Variscan
stages, when both “orogenic” and granite-related ores resulted from a wide metallogenic fertilization of the
Sardinian crustal segment. These events may be tentatively framed in a context of lithospheric delamination,
which triggered production and crustal-scale migration of magmas and fluids along lithospheric shear zones,
widely redistributing ore-forming elements, including (a) new contributions linked to partial melting of
different crustal levels and to crust/mantle interactions, and (b) widespread recycling of elements present in
the pre-Variscan successions (e.g., Pb, Zn, Ba from Cambrian MVT ores of SW Sardinia; REE from Upper
Ordovician paleoplacers in Eastern Sardinia). Variscan crustal fertilization was essential for the post-Variscan
metallogenic stages (Middle Permian-Triassic?), during which new and widespread fluid circulation in the
basement produced, in the context of the breakup of Pangea and the opening of the Tethys (Burisch et al.,
2022), different kinds of low-temperature polymetallic hydrothermal ores (Pb-Zn ± Cu±Ag; Ni-Co-As-Bi-Ag;
Ba-F ± Pb ± Ag), often directly remobilizing previous magmatic-hosted/related ones
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