992 resultados para 336-U1383D
Resumo:
Frankfurter Dialekttheater, Wilhelm Sauerwein: "Der Gräff, wie er leibt und lebt", "Gräff im Grünen", "Der Amerikaner", Carl Malß, Pfeifer: "Die Brunnenfahrt", Sauerwein: Briefe an Wilhelm Rieger (verloren), Collegzeitung, Geplante Sauerwein-Gesamtausgabe
Resumo:
126 Briefe zwischen Max Horkheimer und Leo Löwenthal, Januar - August 1948; 1 Brief von Max Horkheimer an Herbert Marcuse, 1948; 2 Briefe zwischen Theodor W. Adorno und Leo Löwenthal, 1948; 1 Brief von Leo Löwenthal an Samuel H. Flowerman, 15.06.1948; 3 Briefe zwischen Erich Preiser und Leo Löwenthal, 1948; 1 Brief von Max Horkheimer an Howard Wilson, 28.08.1948; 1 Brief von Paul Lazarsfeld an Leo Löwenthal, 26.08.1948; 1 Brief von Käte Hirsch an Leo Löwenthal, [1948]; 1 Brief von Willy Haas an Max Horkheimer, 15.07.1948; 1 Brief von Max Horkheimer an Moses Finley, 16.08.1948; 1 Brief von Max Horkheimer an Robert J. Havighurst, [August 1948]; 1 Brief (Auszug) von Hans Mayer an Max Horkheimer, 23.03.1948; 1 Brief von Julius Schwietering an Max Horkheimer, 18.02.1948; 1 Brief von E. Stein an Max Horkheimer, 26.06.1948;
Resumo:
Fil: Banzato, Guillermo. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
Fil: Banzato, Guillermo. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
Measurements of 87Sr/86Sr ratios of interstitial waters from leg 25, site 245 and leg 38, site 336 of the Deep Sea Drilling Project show that the enrichment of Sr[2+] with depth is caused both by the alteration of volcanic material and by the introduction of strontium derived from calcium carbonate. 87Sr/86 Sr ratios range from 0.70913 to 0.70794 at site 245 and from 0.70916 to 0.70694 at site 336. The low ratios compared with contemporaneous seawater reflect the release of Sr from a volcanic source having, according to material-balance calculations, a 87Sr/86 Sr ratio of about 0.7034 at site 336. At this site the source appears to be volcanic ash and not basaltic basement which acts as a sink for Sr[2+] during in situ low-temperature weathering. The volcanic contribution to the strontium enrichment in the basal interstitial waters varies from <10% at site 245 to >50% at site 336. The remaining Sr[2+] is derived from Sr-rich biogenic carbonate during diagenetic recrystallization to form Sr-poor calcite.
Resumo:
Fil: Banzato, Guillermo. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.