1000 resultados para 128-798
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Ziegenhain, Pfarrer Jost, Kassel, Frankfurter Latern, Persönliche Nachrichten
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2 Briefe zwischen der Buchhandlung Peter Naacher und Max Horkheimer, 1966-1968; 1 Brief von E. Nabulon an Max Horkheimer, 1971; 13 Briefe und Beilage zwischen dem Dozenten Georg Nádor und Max Horkheimer, 1964-1967; 4 Briefe zwischen Cornelia Nass und Max Horkheimer sowie der Beilage: Vortrag von Val. Giscard d'Estaing über "die neue Gesellschaft" Brüssel 1970, 1970-1972; 6 Briefe zwischen Else Nassauer und Max Horkheimer, 1967-1973; 3 Briefe zwischen S.Andhil Fineberg und Max Horkheimer, 1967-1969; 1 Brief von Dr. med. Horst Naujoks an Max Horkheimer, 1963; 3 Briefe von Max Horkheimer an die Zeitschrift Nebelspalter, 1964-1969; 7 Briefe zwischen Max Horkheimer und Carl Nedelmann, 1964; 2 Briefe und Beilage zwischen Dr. Renate Neef-Cramer und Max Horkheimer, 1972; 3 Briefe zwischen Walter Neef und Max Horkheimer, 1965; 1 Brief an Dr. Oskar Negt von Max Horkheimer, 1964; 9 Briefe zwischen Dr. Günther Nenning und Max Horkheimer, 1962-1972; 4 Briefe zwischen der Neuen Deutschen Biographie und Max Horkheimer, 1969-1970; 4 Briefe und Beilage zwischen der Wochenschrift Neue Politik und Max Horkheimer, 1971; 6 Briefe zwischen Joachim Günther und Max Horkheimer, 1969-1970; 10 Briefe zwischen der Neuen Rundschau Rudolf Hartung und Max Horkheimer, 1964-1968; 1 Brief an Heinz Friedrich von Max Horkheimer, 1969; 9 Briefe zwischen Dr. Günther Nenning und Max Horkheimer, 1969-1972; 4 Briefe zwischen dem Rektor Günther Neuhardt und Max Horkheimer, 1970; 7 Briefe zwischen Rexa Neumeister und Max Horkheimer, 1967; 28 Briefe und Beilage zwischen dem Professor Ludwig Neundörfer und Max Horkheimer, 1955-1971; 1 Brief an den Professor John J. Neunaier von Max Horkheimer, 1965; 2 Briefe zwischen der Newton Compton Editori und Max Horkheimer, 1970; 3 Briefe zwischen der New York Times und Max Horkheimer, 1959-1960; 4 Briefe und Beilage zwischen Stephen Ney und Max Horkheimer, 1967; 4 Briefe und Beilage zwischen dem Student Claus Niederberger und Max Horkheimer, 1973; 1 Brief an Dr. Friedrich Niewöhner von Max Horkheimer, 1973; 4 Briefe zwischen dem Professor August Nietschke und Max Horkheimer, 1965; 1 Dankesbrief von N.N. an Maidon Horkheimer, 1963; 1 Brief [Hinweis auf eine Krebstherapie] von N.N. an Max Horkheimer; 1 Brief [gegen den Kommunismus] von N.N. an Max Horkheimer, 1955; 1 Brief [Ansichtskarte, Unterzeichnet mit D.C.] von N.N. an Max Horkheimer, 1953; 1 Telegramm [Mitteilung über Schiffverbindung] von N.N. an Max Horkheimer, 1949; 3 Briefe und Beilage zwischen dem Northern Life Insurance Co. Seattle, Wash. und Max Horkheimer, 1951-1953; 4 Briefe und Beilage zwischen den Nürnberger Nachrichten und Max Horkheimer sowie einem Interview mit Max Horkheimer, 1973; 1 Brief von der Nymphenburger Verlagshandlung an Max Horkheimer, 1968;
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20 Briefe zwischen dem Studenten Iwan Nagel und Max Horkheimer, 1952-1953; 20 Briefe und Beilage zwischen Theodor W. Adorno sowie Max Horkheimer und Iwan Nagel, 1952-1953; Material "Gegen N. aus der NS-Zeit" von Professor Hans Naujoks an Max Horkheimer, 1954; 3 Briefe zwischen dem Professor John U.Nef und Max Horkheimer, 1953; 7 Briefe zwischen der Studentin Dorothee Neff und Max Horkheimer, 1951-1956; 3 Briefe an den Historiker und Sozialwissenschaftler Benjamin Nelson von Max Horkheimer, 1959; 31 Briefe und Beilage zwischen dem Professor Franz L. Neumann und Max Horkheimer, 1950-1954;
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Vorbesitzer: Antonius Forsch de Meiningen; Adolf von Glauburg; Johann Ernst von Glauburg
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2 Briefe zwischen Frederick Pollock und der Southern Counties Gas Company of California (Santa Monica), Dezember 1946; 1 Brief von Frederick Pollock an Pacific Electric Railway Co. (West Los Angeles), 16.05.1946;
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a Balthasare Straubio
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Vorbesitzer: Johann Hieronymus Zum Jungen
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The western Pacific includes many volcanic island arc and backarc complexes, yet multi-isotopic studies of them are rare. Basement rocks of the Sea of Japan backarc basin were encountered at Sites 794,795, and 797, and consisted of basaltic sills and lava flows. These rocks exhibit a broad range in isotopic composition, broader than that seen in any other western Pacific arc or backarc system: 87Sr/86Sr = 0.70369 to 0.70499, 143Nd/144Nd = 0.51267 to 0.51317, 206Pb/204Pb = 17.64 to 18.36. The samples form highly correlated arrays between very depleted mid-ocean ridge basalt (MORB) and the Pacific pelagic sediment fields on Pb-Pb plots. Similarly, on plots of Sr-Pb and Nd-Pb, the Sea of Japan samples lie on mixing curves between depleted mantle and enriched mantle ("EM II"), which is interpreted to be of average crustal or pelagic sediment composition. The source of these backarc rocks appears to be a MORB-like mantle source, contaminated by pelagic sediments. Unlike the Mariana and Izu arc/backarc systems, Japanese arc and backarc rocks are indistinguishable from each other in a Sr-Nd isotope plot, and have similar trends in Pb-Pb plots. Thus, sediment contamination of the mantle wedge appears to control the isotopic compositions of both the arc and backarc magmas. Two-component mixing calculations suggest that the percentage of sediments in the magma source varies from 0.5% to 2.5%.
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The basaltic rocks of Hole 794D drilled during Leg 128 are strongly altered. Microprobe analyses and XRD spectra on small quantities of matter extracted from thin sections show that primary minerals and glassy zones of the groundmass are totally or partially replaced by clay minerals with chlorite/saponite mixed-layer composition whatever the rock sample considered. This mixed-layer was also identified in veins and vesicles where it crystallizes in spheroidal aggregates. The largest veins and vesicles are filled by a zoned deposit: the chlorite/saponite mixed-layer always occupies the central part and is rimmed by pure saponite. Calcite crystallizes in secondary fractures which crosscut the clayey veins and vesicles. Chemographic analysis based on the M+-4Si-3R2+ projection shows that the chemical composition of the saponite component in the mixed-layer is identical to that of the free saponite. This indicates that the clay mineral crystallization was controlled by the chemical composition of the alteration fluids. From petrographic evidence, it is suggested that both chlorite/saponite mixed-layer and free saponite belong to the same hydrothermal event and are produced by a temperature decrease. This is supported by the stable isotopic data. The isotopic data show very little variation: d18O saponite ranges from 13.1 per mil to 13.5 per mil, and dD saponite from -73.6 per mil to -70.0 per mil. d18O calcite varies from +19.7 per mil to +21.9 per mil vs SMOW and d13C from -3.2 per mil to +0.4 per mil vs. PDB. These values are consistent with seawater alteration of the basalt. The formation of saponite took place at 150°-180°C and the formation of calcite at about 65°C.