Results 21 to 30 of about 4,994 (164)
La proposition concessive dans la poésie des troubadours
Resumo: Este estudo visa apresentar as possibilidades da expressão concessiva na poesia dos trovadores dos séculos XII e XIII. De uma figura retórica inicial, a concessão torna-se uma noção gramatical, a partir do século XVII.
Sybille Haefele
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The Judaeo-Provençal tradition of Purim celebrations is to be considered particularly interesting: in fact, most Judaeo-Provençal texts - which constitute a comparatively small corpus - are interpretations of the story of Esther, dating from XIV to XX ...
Erica Baricci
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Du nouveau sur le royaume de Pampelune au IXe siècle
Lévi-Provençal Évariste. Du nouveau sur le royaume de Pampelune au IXe siècle. In: Bulletin Hispanique, tome 55, n°1, 1953. pp.
Lévi-provençal, Évariste +1 more
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M. P. Provençal nadiu. In: Romania, tome 30 n°118-119, 1901. pp.
Meyer, Paul
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Toponymie de la Provence: état des lieux, questions, enjeux et errements [PDF]
The objective of this contribution is not to present the results of new in-depth research on the provençal. It rather aims at raising the awareness of an informed and curious -but non-specialized -audience to the different aspects of the toponymy,
Denis ROUX
doaj
Brunel Clovis. Provençal sebenc. In: Romania, tome 87 n°345, 1966. pp.
Brunel, Clovis
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Brunel Clovis. Provençal girval. In: Romania, tome 77 n°306-307, 1956. pp.
Brunel, Clovis
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Long‐Term Deformation in the Alpine‐Provence Foreland Constrained by In Situ Calcite U‐Pb Dating
Abstract The evolution of the Alpine‐Provence foreland is characterized by multiple deformation phases since the Mesozoic, representing successive compressional and extensional episodes. The precise timing and spatial evolution of these deformation phases remain poorly constrained due to the lack of absolute geochronological data. Here, we present U–Pb
Dorian Bienveignant +12 more
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Brunel Clovis. Provençal manbes, marves. In: Romania, tome 51 n°204, 1925. pp.
Brunel, Clovis
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Abstract The paleomagnetism of Miocene calc‐alkaline volcanics and sediments from Sardinia has firmly showed that the Corsica‐Sardinia microplate rotated 50°–60° counterclockwise (CCW) with respect to Europe between 21 and 15 Ma, during its drift from the Provencal margin. However, Permian to Eocene rocks from central‐south Sardinia revealed higher (up
Gaia Siravo +3 more
wiley +1 more source

