991 resultados para Knorr, Karl
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Musik von F. Halevy. Nach dem Franz. von Casimir und Germain Delavigne
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235 Briefe zwischen Leo Löwenthal und Max Horkheimer, 1948 - 1950; 4 Briefe zwischen Frederick Pollock und Leo Löwenthal, 1948 - 1949; 1 Brief von Frederick Pollock an Karl Wittfogel, [1949]; 1 Brief von Leo Löwenthal an Mark Vosk, 13.08.1949; 3 Briefe zwischen Jeremiah Kaplan und Leo Löwenthal, 1949; 2 Briefe von Paul F. Lazarsfeld an Leo Löwenthal, 1949/1950; 1 Brief von Erik Rinde an Paul F. Lazarsfeld, 19.09.1950; 1 Brief von Leo Löwenthal an Jim Farrell, 25.01.1949; 1 Brief von Clement S. Mihanovich an Leo Löwenthal, 14.01.1949; 1 Brief von David Riesman an Leo Löwenthal, 06.11.1950; 1 Brief von Leo Löwenthal an Katherine Taylor, 27.05.1950; 1 Brief vom Rektor der Johann Wolfgang Goethe-Universität (Frankfurt am Main) an J. W. Thompson, 11.03.1950;
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Briefwechsel zwischen Max Horkheimer, Frederick Pollock und Karl August und Olga Wittfogel; 1 Brief von Karl August Wittfogel an Stephen Duggan, 02.08.1936; 2 Briefe an Max Horkheimer von Karl August Wittfogel, November 1937; 1 Brief von Karl August Wittfogel an Carter, 16.07.1936; 1 Brief an den American Consul General (Tientein, China) von Max Horkheimer, 03.04.1936; 1 Brief von Max Horkheimer an Owen Lattimore, 28.12.1935;
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[National-Theater zu Frankfurt am Main]
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Signatur des Originals: S 36/F03527
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von Heinrich Levy-Koref
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Chemical and mineralogical compositions of ferromanganese oxide coatings on rocks dredged from the New England Seamounts, the Sierra Leone Rise and the Mid-Atlantic Ridge near the Equator have been determined in an investigation of regional differences in Atlantic ferromanganese deposits. Most encrustations are clearly of hydrogenous origin, consisting mainly of todorokite and delta MnO2, but several recovered from the equatorial fracture zones may be hydrothermal accumulations. Differences in the chemistry of the water column and in growth rates of the ferromanganese coatings may be important in producing this regional contrast in composition. Fine-scale changes in element abundances within the encrustations indicate that the nature of the substrate has little influence on compositional variations.