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1	Überlieferung und Quelle der Reinoldlegende ... Ostendorf, Franz, January 1911 (has links) Inaug.-Diss.--Münster. / Lebenslauf. Published in full in Forschungen und Funde, hrsg. von F. Jostes. Bd. III, Hft. 3 (2 p. l., 70 p.)
2	A dramatic adaptation of Rabelais in the seventeenth century Les aventures et le mariage de Panurge (1674) by Pousset de Montauban, Chevalier, Marion Frances, January 1933 (has links) Portion of Thesis (Ph. D.)--John Hopkins University, 1933. / Vita. Reprinted from the John Hopkins studies in Romance literatures and languages, extra volume VI." Includes only the author's study of Montauban's life and dramatic works. Bibliography: p. 189-196.
3	Ketzer, Konsuln und Büsser die städtischen Eliten von Montauban vor dem Inquisitor Petrus Cellani (1236/1241) Feuchter, Jörg January 2006 (has links) Zugl.: Berlin, Humboldt-Univ., Diss., 2006
4	Der erste teil der chanson der IIII fils Aymon nach der Oxforder handschrift Laud 637 ... Quegwer, Friedrich, January 1914 (has links) Inaug.-diss.--Greifswald. / Lebenslauf. "Einleitung" (p. [5]-11) includes bibliographical notes.
5	Geology, geochemistry and genesis of Montauban lead-zinc deposits Prabhu, Mohan Keshav. January 1981 (has links) Lithogeochemical investigations were carried out in and around the Montauban polymetallic deposits of the Grenville Province, Quebec. A number of chemical criteria used to distinguish sedimentary and igneous protoliths for the ore host rocks were tested and found to be weak in their discriminating capabilities. Critically evaluated chemical criteria show that the protoliths for quartzofeldspathic gneisses, quartz-rich rocks, and host rocks were mainly siliceous sediments and intercalated carbonate lenses. Hornblende gneisses of the Montauban area are orthogneisses. They and other orthoamphibolite rocks in the study area have a tholeitic affinity. Incompatible element chemistry suggests that they were formed in an island-arc (including back-arc) environment. / Alteration associated with the Montauban Pb-Zn deposits is weak and has a narrow lateral extension with erractic chemical halos close to the ore-bearing zones. A CaO-rich zone extends up to 140 m laterally to the east from the calc-silicate ore zone, and an anomalous MgO zone extends on both sides of the cordierite-anthophyllite ore zone into the quartzofeldspathic gneisses. The cordierite-anthophyllite gneiss host rock is more anomalous in Zn, Pb, Cu and Au than the calc-silicate host rock. Erractic high concentrations of Zn and Au occur within the quartzofeldspathic gneisses close to both ore-bearing zones. Copper and Au occur at slightly greater depths than Zn and Pb within the deposits. / The Montauban Pb-Zn deposits were formed in a mainly sedimentary environment, probably by exhalative processes, and were metamorphosed to the almandine-amphibolite facies with the enclosing sediments.
6	Die jüngere Redaktion der Chanson Renaut de Montauban nach der Pariser und Londoner Handschrift und ihr Verhältnis zur älteren Version ... Schumacher, Kurt, January 1914 (has links) Thesis--Greifswald. / Cover title. Vita. Includes bibliographical references.
7	Geology, geochemistry and genesis of Montauban lead-zinc deposits Prabhu, Mohan Keshav. January 1981 (has links) No description available.
8	Metamorphosed volcanogenic Pb-Zn deposits at Montauban, Quebec Stamatelopoulou-Seymour, Karen. January 1975 (has links) No description available. Rocks, Metamorphic.
9	Metamorphosed volcanogenic Pb-Zn deposits at Montauban, Quebec Stamatelopoulou-Seymour, Karen. January 1975 (has links) No description available. Rocks, Metamorphic.
10	The precambrian geology of the Montauban area, Quebec. Pyke, D. R. January 1967 (has links) No description available. Geology, Stratigraphic -- Precambrian.

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