{[N.N.], Szenenfoto, Gruppenbildnis, in: Hurra, mir erwe, Mainz: Stadttheater, 1932/33

Signatur des Originals: S 36/F11331

Na 1 Nachlass Max Horkheimer, 619 - Unterlagen zu "Empiriokritizismus", "Neukantianismus", "Phänomenologie" und zur "Lebensphilosophie" (p. VIII 29-VIII 33)

"Einleitung in die Philosophie", Wintersemester 1932/33, eigenhändige Notizen, 1 Heft, 12 Blatt, davon 5 leer, und 8 zusätzliche Blätter; Zwei Aufsätze vor 1933 (enthält: "Über Kants Philosophie", Typoskript mit eigenhändigen Korrekturen, 8 Blatt. Mit 1 Blatt von Theodor W. Adorno an Max Horkheimer, 29.04.1954 (GS 11, S. 202-208; "Nicolai Hartmann", ca 1931, Typoskript mit eigenhändigen Korrekturen, 6 Blatt (GS 2, S. 172-176)); "Zur Emanzipation der Philosophie von der Wissenschaft" (GS 10, S. 334-419). Über Empiriokritizismus (Mach), Neukantianismus (Cohen), Phänomenologie (Husserlm Scheler), Lebensphilosophie (Bergson), nach 1927 - vor 1933; a) Typoskript mit eigenhändigen Korrekturen, gebunden, 114 Blatt, b) Typoskript mit handschriftlichen Korrekturen, 109 Blatt; Über Erkenntnistheorie und Gestalttheorie (GS 11, S. 22-69), Manuskript, in 2 Heften (Heft 1, 96 Blatt; Heft 2, 32 Blatt);

Na 1 Nachlass Max Horkheimer, 578 - Korrespondenzen mit Friedrich (Frederick) Pollock (p. VI 33, 1-360)

1 Brief von Margot von Mendelssohn an Alice H. Maier, 31.12.1942; 1 Drucksache von Fortune [amerikanische Zeitschrift], Dezember 1942; 1 Brief von Frederick Pollock an Bay District Motors Co. (Santa Monica), 17.09.1942; 3 Briefe zwischen Robert M. MacIver und Frederick Pollock, 1943; 2 Briefe zwischen Frederick Pollock und David Rosenblum, 1943; 1 Brief von Robert S. Lynd an Frederick Pollock, 26.04.1943; 1 Brief von Sheed and Ward Inc. (New York) an Max Horkheimer, 08.02.1943; 1 Telegramm von Juliane Favez an Frederick Pollock, 06.02.1943; 1 Brief von Max Horkheimer an das Federal Bureau of Investigation (Los Angeles), 13.01.1943; 1 Brief von Hannah Tillich an Frederick Pollock, 11.01.1943;

Na 1 Nachlass Max Horkheimer, 579 - Korrespondenzen mit Friedrich (Frederick) Pollock (p. VI 33, 361-548)

3 Briefe zwischen Robert M. Mac Iver und Frederick Pollock, 1943; 1 Brief von dem Office of Strategic Services (Washington) an Frederick Pollock, 14.09.1943; 1 Brief von dem U. S. Government Printing Office (Washington) an Frederick Pollock, 01.09.1943; 1 Brief von Frederick Pollock an Franco Bruno Averardi, 19.07.1943; 1 Brief von Frederick Pollock an Leo Löwenthal, 15.07.1943; 1 Brief von Emil E. Mayer an F. Landauer, 28.05.1943; 2 Briefe zwischen Frederick Pollock und Erich Rosenberg, 1943; 1 Brief von Frederick Pollock an George Mintzer, 12.05.1943; 1 Brief von Iago Galdstone (Arzt) an Frederick Pollock, 10.05.1943; 1 Brief von Frederick Pollock an Theodor W. Adorno, 11.05.1943; 1 Brief von Frederick Pollock an den British Information Services (New York), 11.05.1943;

Ms. lat. oct. 33 - Logica

Vorbesitzer: Martinus Christianus

Ms. lat. qu. 33 - Geschichte des Papsttums. Schweiz, Neapel. Hugenotten.

Vorbesitzer: Johann Maximilian Zum Jungen

Geochemistry and mineralogy at DSDP Holes 61-462, 61-462A and 33-315A

Sedimentary rocks of Barremian through early Maestrichtian age recovered on Deep Sea Drilling Project Leg 61 had their principal source in the complex of igneous rocks with which they are interlayered in the Nauru Basin. Relict textures and primary sedimentary structures show these Cretaceous sediments to be of hyaloclastic origin, in part reworked and redeposited by slumps and currents. The dominant composition now is smectite, but locally iron, titanium, and manganese oxides, plagioclase, pyroxene, analcime, clinoptilolite, chalcedonic quartz, cristobalite, amphibole, nontronite, celadonite, and pyrite are also present. The mineral assemblages and the geochemistry reflect the original basaltic composition and its subsequent alteration by one or more processes of submarine weathering, authigenesis, hydrothermal circulation, and contact metamorphism. Hyaloclastitic sandstone, siltstone, and breccia within the sheet flows below 729 meters sub-bottom depth have Barremian fossils, thus establishing the age of the lower, or extrusive, complex of post-ridge-crest volcanism. Similar hyaloclastites between 564 and 729 meters are invaded by hypabyssal sills of the upper igneous complex, and fossil ages of Albian or Cenomanian set an older limit to the age of that second post-ridge-crest episode. Cenomanian to early Campanian sedimentary rocks between 490 and 564 meters have a substantial contribution of clays of submarine-weathered-basalt origin, as well as hydrothermal and pelagic components. The interval of reworked hyaloclastitic siltstone, sandstone, and breccias between 450 and 490 meters is of late Campanian and early Maestrichtian age. These sediments probably formed from glassy basalt that fragmented upon eruption nearby, when sills were being emplaced. In addition to pelagic elements, these Upper Cretaceous volcanogenic sediments include redeposited material of shallow-water origin, apparently derived from the Marshall Islands.