Ms. lat. qu. 115 - Relazionen, satirische Schriften und Gedichte

Die Foliierung geht nur bis Bl. 323; zusätzlich gibt es die Blätter 5a, 115a und 271a; das Blatt 299 wurde bei der Foliierung ausgelassen.

Ms. hebr. oct. 115 - [Sammelband in 2 Teilen: Handschriftenkonvolut]

Vorbesitzer: Abraham Merzbacher

Das Erdbeben im Jahre 115 in Palästina

Samuel Krauss

Na 1 Nachlass Max Horkheimer, 28 - Korrespondenzen mit u.a. Siegfried Kracauer (p. I 14, 115-368)

95 Briefe und Beilagen zwischen Siegfried Kracauer und Max Horkheimer, 1936-1949; 2 Briefe zwischen Else Staudinger vom American Committee for Refugee Scholars, Writers and Artists New York und Max Horkheimer, 10.07.1945, 24.07.1945; 2 Briefe zwischen Meyer Schapiro und Siegfried Kracauer 19.11.1937, 03.12.1937; 2 Briefe von Leo Löwenthal an Schapiro Meyer, 1940, 1941; 1 Brief und 1 Beilage von Max Horkheimer an A. Schütz, 02.08.1940; 1 Brief von Max Horkheimer an Trude Krautheimer, 30.07.1940; 1 Brief von Max Horkheimer an das Hebrew Sheltering and Immigrant Aid New York, 10.06.1940; 2 Briefe ziwschen dem Department of State Washington und Max Horkheimer, 05.04.1939, 1939; 2 Briefe zwischen Betty Drury Max Horkheimer, 05.11.1938, 07.11.1938; 2 Briefe zwischen Margaret Krafft und Max Horkheimer, 1938, 1939; 1 Brief von Gertrud Kurth-Kieslinger an Max Horkheimer, 02.10.1939; 2 Briefe zwischen Werner Kraft und Max Horkheimer, 19.01.1940, 01.03.1940; 1 Brief und 1 Beilage von Friedrich Krause an Max Horkheimer, 05.01.1939; 2 Briefe zwischen Karl Krayl und Max Horkheimer, 201.10.1937, 25.11.1937; 11 Briefe zwischen Ernst Krenek und Max Horkheimer, 1937-1941; 1 Brief von S. Krezel an Max Horkheimer, 12.02.1936; 1 Brief von Charles I. Krieger an Max Horkheimer, 01.08.1940; 1 Brief von H. Kronstein an Max Horkheimer, 20.05.1935; 3 Briefe zwischen Germaine Krull und Max Horkheimer, 1934, 06.09.1937, 1937; 3 Briefe zwischen Lawrence S. Kubie Sekretär der American Psychoanalytic Association, New York und Max Horkheimer, 11.05.1938, 1938; 5 Briefe und Beilagen zwsichen Julius Kühl und Max Horkheimer, 18.10.1939-1940; 1 Brief von Max Horkheimer an Herr Guggenheim, 20.02.1940; 1 Brief von Julius Kühl an die ESKA, 31.03.1945; 4 Briefe zwischen B. Kugelmann und Max Horkheimer, 1934, 1938, 1939; 1 Brief von Georg Kunzel an Max Horkheimer, 01.08.1930;

Ms. Praed. 115 - De vita Christiana

Vorbesitzer: Dominikanerkloster Frankfurt am Main

Ms. Barth. 115 (Ausst. 27) - Legenda aurea

Vorbesitzer: Johannes de Dusburg; Brune-Kütze-Legat; Bartholomaeusstift Frankfurt am Main

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 115 - Bitte um Versendung zweier Briefe an Madame Herbigny

u.a.: Hübbe;

Ms.Ff.F.Stoltze 3. 115 - Brief von Carl Heinz an Friedrich Stoltze

Glückwunsch (Gedicht)

Noble metal abundances in ODP Leg 115 basalts (Table 1)

A comparison of 50 basalts recovered at Sites 706, 707, 713, and 715 along the Reunion hotspot trace during Ocean Drilling Program Leg 115 in the Indian Ocean shows that seafloor alteration had little effect on noble metal concentrations (Au, Pd, Pt, Rh, Ru, and Ir), determined by inductively coupled plasma-mass spectrometry (ICP-MS), which generally tend to decrease with magma evolution. Their compatible-element behavior may be related to the precipitation of Ir-Os-based alloys, chromite, sulfides, and/or olivine and clinopyroxene in some combination. The simplest explanation indicates silicate control of concentrations during differentiation. Basalts from the different sites show varying degrees of alkalinity. Noble metal abundances tend to increase with decreasing basalt alkalinity (i.e., with increasing percentages of mantle melting), indicating that the metals behave as compatible elements during mantle melting. The retention of low-melting-point Au, Pd, and Rh in mantle sulfides, which mostly dissolve before significant proportions of Ir-Os-based alloys melt, explains increasing Pd/Ir ratios with decreasing alkalinity (increasing melting percentages) in oceanic basalts. High noble metal concentrations in Indian Ocean basalts (weighted averages of Au, Pd, Rh, Pt, Ru, and Ir in Leg 115 basalts are 3.2, 8.1, 0.31, 7.3, 0.22, and 0.11 ppb, respectively), compared with basalts from some other ocean basins, may reflect fundamental primary variations in upper- mantle noble metal abundances

Isotope ratios of basalts from ODP Leg 115 holes (Table 1)

Strontium, neodymium, and lead isotope ratios are reported for 13 Leg 115 basalts as well as 3 basalts from Texaco drill hole SM-1 on the Mascarene Plateau. The 87Sr/86Sr ratios and eNd range from 0.70330 to 0.70439 and 5.5 to 7.4, respectively, although 87Sr/86Sr ratios higher than 0.70383 are found only in SM-1 basalts. The high 87Sr/86Sr values are thought to reflect seawater Sr in secondary phases, although all samples were strongly leached in HC1 before analysis. 206Pb/204Pb ratios range from 18.53 to 18.80, and sho high 207Pb/204Pb and 208Pb/204Pb ratios relative to 206Pb/204Pb ratios, typical of Indian Ocean mid-ocean ridge (MORB) and oceanic-island basalts (OIB). Isotopic compositions of Leg 115 basalts generally fall between fields for MORB and Reunion Island basalts, consistent with the conclusion drawn from geochronological studies that Deccan flood basalt volcanism, the Chagos-Laccadive Ridge, and the Mascarene Plateau are all products of the Reunion mantle plume. Isotopic compositions of magmas produced by this plume have varied systematically with time in the direction of less "depleted," less MORB-like isotopic signatures. This compositional change has been accompanied by a decrease in eruption rate. We interpret Deccan volcanism as the voluminous beginning of the plume. Reduced entrainment of asthenosphere following melting of the plume head resulted in less MORB-like isotope ratios in magmas and a decrease in eruptive activity with time.