998 resultados para Ligerz, Heinrich von.


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"Pareto und die 'Frankfurter' Solziologische Schule" (GS 11, S. 196-201). Über Gottfried Salomon und Heinz Otto Ziegler, 26.10.1929, Typoskript, 7 Blatt; Teil eines Manuskripts für eine Vorlesung im Volksbildungsheim, Geschichtsphilosophie, Psychoanalyse, Wintersemester 1929/30, Manuskript, 1 Heft, 15 Blatt, und 1 zusätzliches Blatt; Friedrich Pollock: Kollegheft zur Vorlesung von Max Horkheimer "Einführung in die Philosophie und ihre Geschichte", Sommersemester 1930, eigenhändige Notizen, 1 Heft, 6 Blatt; Friedrich Pollock: Kollegheft zu Übungen von Max Horkheimer über Grundlagen der Sozialphilosophie; vor allem über Heinrich Rickert, Max Weber und Max Scheler, Wintersemester 1930/31 im Volsbildungsheim, eigenhändige Notizen, 1 Heft, 24 Blatt, und 13 zusätzliche Blätter, ausserdem beiliegend: G. Biehahn: Protokoll zum Seminar von Max Horkheimer über Geschichtsphilosophie, Typoskript, 3 Blatt; Friedrich Pollock: Notizen zu den 'Sozialphilosophischen Übungen' von Max Horkheimer, über Hegel und Marx, Sommersemester 1931, 18 Blatt; "Hegel und das Problem der Metaphysik" (GS 2, S. 295-308; GS 11, S. 221-229), 1932, Typoskript mit eigenhändigen Korrekturen, 23 Blatt; sowie Stichworte zu Hegel, neuere Metaphysik, historischer Materialismus, Typoskript, 1 Blatt;

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... von Heinrich Kinderlieb [d.i. Heinrich Hoffmann]

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nach der Natur gezeichnet und in 26 Blättern hrsg. von Joseph Nicolaus Peroux. In Kupfer gestochen durch Heinrich Ritter. Nebst einer histor. Erläuterung von Vogt

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Heinrich Stoltze in New York

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von Max Jungmann

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Vorbesitzer: Heinrich Anton Cornill-d'Orville

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Sediment dynamics in limnic, fluvial and marine environments can be assessed by granulometric and rock-magnetic methodologies. While classical grain-size analysis by sieving or settling mainly bears information on composition and transport, the magnetic mineral assemblages reflect to a larger extent the petrology and weathering conditions in the sediment source areas. Here, we combine both methods to investigate Late Quaternary marine sediments from five cores along a transect across the continental slope off Senegal. This region near the modern summer Intertropical Convergence Zone is particularly sensitive to climate change and receives sediments from several aeolian, fluvial and marine sources. From each of the investigated five GeoB sediment cores (494-2956 m water depth) two time slices were processed which represent contrasting climatic conditions: the arid Heinrich Stadial 1 (~ 15 kyr BP) and the humid Mid Holocene (~ 6 kyr BP). Each sediment sample was split into 16 grain-size fractions ranging from 1.6 to 500 µm. Concentration and grain-size indicative magnetic parameters (susceptibility, SIRM, HIRM, ARM and ARM/IRM) were determined at room temperature for each of these fractions. The joint consideration of whole sediment and magnetic mineral grain-size distributions allows to address several important issues: (i) distinction of two aeolian sediment fractions, one carried by the north-easterly trade winds (40-63 µm) and the other by the overlying easterly Harmattan wind (10-20 µm) as well as a fluvial fraction assigned to the Senegal River (< 10 µm); (ii) identification of three terrigenous sediment source areas: southern Sahara and Sahel dust (low fine-grained magnetite amounts and a comparatively high haematite content), dust from Senegalese coastal dunes (intermediate fine-grained magnetite and haematite contents) and soils from the upper reaches of the Senegal River (high fine-grained magnetite content); (iii) detection of partial diagenetic dissolution of fine magnetite particles as a function of organic input and shore distance; (iv) analysis of magnetic properties of marine carbonates dominating the grain-size fractions 63-500 µm.