1000 resultados para 982.83


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veröffentlicht in: Schopenhauer, Arthur : Arthur Schopenhauers sämtliche Werke - München : Piper - Bd. 14 : Der Briefwechsel Arthur Schopenhauers ; 1 (1799 - 1849), Nr. 9;

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1 Brief von Eugen Ripp an Max Horkheimer, 1952; 24 Briefe zwischen Professor Jürgen Habermas und Max Horkheimer, 1960-1971; 3 Briefe zwischen Notar Häfele und Max Horkheimer, 1950; 7 Briefe zwischen Professor Georg W. F. Hallgarten und Max Horkheimer, 1959; 35 Briefe zwischen Professor Walter Hallstein und Max Horkheimer, 1946-1967; 8 Briefe zwischen der Staatssekretärin Hildegard Hamm-Brücher und Max Horkheimer, 1968-1969;

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u.a. Frankfurter Zeitung; Politik; Bildnis Schopenhauer;

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Beiträge zur Frankfurter Latern

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Vorbesitzer: Bartholomaeusstift Frankfurt am Main

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Signatur des Originals: S 36/F04199

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Signatur des Originals: S 36/F04200

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Die beiden römisch gezählten Seiten sind eine lose Beilage.

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Vorbesitzer: Bernhard Diell

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Trägerband: Ms. Barth. 18; Vorbesitzer: Bartholomaeusstift Frankfurt am Main

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The Iowa State University Bulletin is a general catalog of information regarding fees, curricula and related policies and procedures.

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The D/H, 18O/16O and 87Sr/86Sr ratios of the basaltic basement from the Leg 83 section of DSDP Hole 504B show that in that area the oceanic crust has experienced intensive but not pervasive alteration. Isotope ratios of the basalts are very heterogeneous because of an input of oxygen, hydrogen, and strontium from seawater. The hydrogen isotopic composition of many samples displays the complete thermal history of the water-rock interactions. High-temperature mineral formations (actinolites, epidotes, and chlorites) were overgrown by a mineralization at lower temperatures (mixedlayer smectites, iddingsites, and smectites) during successive stages of cooling of the oceanic crust by cold seawater. From 87Sr/86Sr data bulk water/rock ratios up to 5:1 have been calculated. There is evidence that some primary minerals like high-An plagioclases contain oxygen from altered basalts. We have discussed the probability that there existed a seawater/crust interface, now at a depth of 620 m sub-basement, during the high-temperature water/rock interactions. This interface was covered during later magmatism by thick flows, pillow lavas, and intrusives.