Das Testament unter der Benennung einer Erbschaft : nach rabbinischen Quellen ; Hefte 1-6

Levi Bodenheimer

Ewaso Ngiro and Meru Ecosystems Elephant Corridors: Site 1-6

7 maps illustrating the elephant corridors in different sites of Ewaso Ngiro, Kenya.

The mobility of Nb in rutile-saturated NaCl- and NaF-bearing aqueous fluids from 1-6.5 GPa and 300-800 °C

Rutile (TiO2) is an important host phase for high field strength elements (HFSE) such as Nb in metamorphic and subduction zone environments. The observed depletion of Nb in arc rocks is often explained by the hypothesis that rutile sequesters HFSE in the subducted slab and overlying sediment, and is chemically inert with respect to aqueous fluids evolved during prograde metamorphism in the forearc to subarc environment. However, field observations of exhumed terranes, and experimental studies, indicate that HFSE may be soluble in complex aqueous fluids at high pressure (i.e., >0.5 GPa) and moderate to high temperature (i.e., >300 degrees C). In this study, we investigated experimentally the mobility of Nb in NaCl- and NaF-bearing aqueous fluids in equilibrium with Nb-bearing rutile at pressure-temperature conditions applicable to fluid evolution in arc environments. Niobium concentrations in aqueous fluid at rutile saturation were measured directly by using a hydrothermal diamond-anvil cell (HDAC) and synchrotron X-ray fluorescence (SXRF) at 2.1 to 6.5 GPa and 300-500 degrees C, and indirectly by performing mass loss experiments in a piston-cylinder (PC) apparatus at similar to 1 GPa and 700-800 degrees C. The concentration of Nb in a 10 wt% NaCl aqueous fluid increases from 6 to 11 mu g/g as temperature increases from 300 to 500 degrees C, over a pressure range from 2.1 to 2.8 GPa, consistent with a positive temperature dependence. The concentration of Nb in a 20 wt% NaCl aqueous fluid varies from 55 to 150 mu g/g at 300 to 500 degrees C, over a pressure range from 1.8 to 6.4 GPa; however, there is no discernible temperature or pressure dependence. The Nb concentration in a 4 wt% NaF-bearing aqueous fluid increases from 180 to 910 mu g/g as temperature increases from 300 to 500 degrees C over the pressure range 2.1 to 6.5 GPa. The data for the F-bearing fluid indicate that the Nb content of the fluid exhibits a dependence on temperature between 300 and 500 degrees C at >= 2 GPa, but there is no observed dependence on pressure. Together, the data demonstrate that the hydrothermal mobility of Nb is strongly controlled by the composition of the fluid, consistent with published data for Ti. At all experimental conditions, however, the concentration of Nb in the fluid is always lower than coexisting rutile, consistent with a role for rutile in moderating the Nb budget of arc rocks.

Na 1 Nachlass Max Horkheimer, 674 - Forschungsprojekte über Antisemitismus, Vorurteil, Autorität: Einzeluntersuchungen (p. IX 141.1-24- IX 142.1-6)

Bettelheim, Bruno; Janowitz, Morris: "A Study on Anxiety and Social Aggression Among Different Groups of War Veterans", 1945-1947; Über die Anfälligkeit der Veteranen für antisemitische Propaganda, Typoskript, englisch, 1 Blatt; "Preliminary Study on the Evaluation of Intolerance Propaganda". Typoskript, 29 Blatt; "Isolationg the Patterns of Intolerance". Typoskript, 30 Blatt; "Distribution of Ethic Intolerance". Typsokript, 18 Blatt; "The Social Characteristics of the Intolerant". Typoskript, 22 Blatt; "Addendum to Social Characteristics of the Intolerant". Typoskript, 16 Blatt; "Impact of War Experiences". Typoskript, 26 Blatt; "Pattern on Sterepotypes". Typoskript, 14 Blatt; "Appendix No. 1: Schedule of Questions Employed in Interview". Typoskript, 6 Blatt; "Appendix No. 2: The Verteran´s Comment on the Interview Situation". Typoskript, 7 Blatt; "Preliminary Report of the Evaluation of Tolerance Propaganda". Typoskript, 19 Blatt; Einleitung zur Beschreibung des Forschungsprojekts, Typoskript, englisch, 1 Blatt; "Instructions for Interviewers". Typoskript, 2 Blat; "Questionaire". Typoskrip, 10 Blatt; "Prupose of the Investigation". Typoskript, 4 Blatt; "Schedule for Interviewers". Typoskript, 6 Blatt; "Appendix: Chicago Veterans Project". Typoskript, 3 Blatt; Memodanden zu Sitzungen mit Bruno Bettelheim, Edward Shils und Theodor W. Adorno; Memorandum 03.04.1945, Typoskript, 2 Blatt; Memorandum 15.03.1945; a) Typoskript, 3 Blatt; b) Typoskript, 4 Blatt; Memorandum 07.03.1945; a) Typoskript, 5 Blatt; b) Typoskript, 6 Blatt; University of Chicago: 1 Brief an Max Horkheimer, Chicago, 29.10.1945; University of Chicago, 1 Brief an Edward Shils undBruno Bettelheim, Chicago, 05.07.1945; Fine, Benjamin: "For Education against Intolerance and Prejudice"; Sonderdruck aus: The Menorah Journal, 1944, Vol. XXXII, No. 2, S. 161-180; Drucksachen, Materialien, 10 Blatt; Ackerman, Nathan W.: zum 'Psychoanalyst Project', 1945-1946; "Towards a Dynamic definition of Anti-Semitism". Typoskript, 13 Blatt; "The Use of Psychoanalytic Case Histories for the Study of Anti-Semitism". Typoskript, 14 Blatt; "Case Material Summary", Tabelle, 5 Blatt; "From for the Collection of Clinical Data on Anti-Minority and Anti-Semitic Attitudes". Als Typoskript vervielfältigt, 5 Blatt; "Case 2". Typoskript, 5 Blatt; "Case 24". Typoskript, 8 Blatt;

Na 1 Nachlass Max Horkheimer, 685 - "Post War Antisemitism in Germany" (p. IX 147.1-6)

Gurland, A.R.L.: "Fight against Antisemitism within the Framwork of Germany's Education for Democracy. Draft Program", 1947. Als Typoskript vervielfältigt, 62 Blatt; Horkheimer, Max: "Momorandum on Post-War Antisemitism in Germany", 31.05.1945. Typoskript, 1 Blatt; Massing, Paul W.; Gurlach, A.R.L.: 2 Briefe mit Unterschrift an Max Horkheimer, ohne Ort, 1944; 1 Brief von Max Horkheimer, ohne Ort, 05.10.1944, 11 Blatt; Massig, Paul W.; Gurlach A.R.L.: "Some Remarks on Leo Löwenthals Memorandum" [September 1944]. Typoskript, 14 Blatt; [Löwenthal, Leo?]: "Post-War Antisemitism in Germany", a) Typoskript, 21 Blatt; b) Typoskript, 29 Blatt; Peck, Georg: "On the Problem of Antisemitism in Post-War Germany", 28.07.1943. Typoskript, 12 Blatt;

Geological map of HANSSONHORNA, Heimefrontfjella, Antarctica (Scale 1:25,000)

Topographic data of this geological map were obtained through stereoscopic aerial photo interpretation. The photogrammetric photo flights were undertaken in 1986 by the Institut für Angewandte Geodäsie, Frankfurt. Horizontal ground control points required for aerial photo interpretation were determined by means of Doppler satellite observation during the 2nd German Neuschwabenland Expedition 1985/86. Vertical ground control points were taken from unpublished map drafts at 1:100 000 scale by Norsk Polarinstitutt, Oslo. The elevation above mean sea level was transferred to Heimefrontfjella barometrically. For this reason assertions concerning the absolute elevation (referred to sea level) are uncertain. Contours and spot heights presented on the map were obtained from the photogrammetric evaluation of the photography taken in 1986; relative elevation data (hight differences) are accurate to approximately ±10 m.

Beck, Heinrich/Ismael Quiles (Editores) Entwicklung zur Menschlichkeit durch Begegnung westlicher und östlicher Kultur: Akten d. IV Interkontinentalen Kolloquiums zur Philos. In-sistenzanthropologie, 1 . - 6 . September 1986 an d. Univ. Bamberg, Frankfurt am Main; Bern; New York; París: Lang, 1988 (Schriften zur Tríadik und Ontodynamik; Band 1)

Fil: Matuschka, Daniel von.

Geological map of RYGHNUTEN, Heimefrontfjella, Antarctica (Scale 1:25,000)

Topographic data of this geological map were obtained through stereoscopic aerial photo interpretation. The photogrammetric photo flights were undertaken in 1986 by the Institut für Angewandte Geodäsie, Frankfurt. Horizontal ground control points required for aerial photo interpretation were determined by means of Doppler satellite observation during the 2nd German Neuschwabenland Expedition 1985/86. Vertical ground control points were taken from unpublished map drafts at 1:100 000 scale by Norsk Polarinstitutt, Oslo. The elevation above mean sea level was transferred to Heimefrontfjella barometrically. For this reason assertions concerning the absolute elevation (referred to sea level) are uncertain. Contours and spot heights presented on the map were obtained from the photogrammetric evaluation of the photography taken in 1986; relative elevation data (hight differences) are accurate to approximately ±10 m.

Geological map of WORSFOLDFJELLET, Heimefrontfjella, Antarctica (Scale 1:25,000)

Topographic data of this geological map were obtained through stereoscopic aerial photo interpretation. The photogrammetric photo flights were undertaken in 1986 by the Institut für Angewandte Geodäsie, Frankfurt. Horizontal ground control points required for aerial photo interpretation were determined by means of Doppler satellite observation during the 2nd German Neuschwabenland Expedition 1985/86. Vertical ground control points were taken from unpublished map drafts at 1:100 000 scale by Norsk Polarinstitutt, Oslo. The elevation above mean sea level was transferred to Heimefrontfjella barometrically. For this reason assertions concerning the absolute elevation (referred to sea level) are uncertain. Contours and spot heights presented on the map were obtained from the photogrammetric evaluation of the photography taken in 1986; relative elevation data (height differences) are accurate to approximately ±10 m.

Geological map of JUCKESKAMMEN, Heimefrontfjella, Antarctica (Scale 1:25,000)

Topographic data of this geological map were obtained through stereoscopic aerial photo interpretation. The photogrammetric photo flights were undertaken in 1986 by the Institut für Angewandte Geodäsie, Frankfurt. Horizontal ground control points required for aerial photo interpretation were determined by means of Doppler satellite observation during the 2nd German Neuschwabenland Expedition 1985/86. Vertical ground control points were taken from unpublished map drafts at 1:100 000 scale by Norsk Polarinstitutt, Oslo. The elevation above mean sea level was transferred to Heimefrontfjella barometrically. For this reason assertions concerning the absolute elevation (referred to sea level) are uncertain. Contours and spot heights presented on the map were obtained from the photogrammetric evaluation of the photography taken in 1986; relative elevation data (hight differences) are accurate to approximately ±10 m.