Ms.Ff.F.Stoltze 3. 140 - Brief von Heinrich Hoffmann an Friedrich Stoltze

Dank für die Gratulation in der Frankfurter Latern

Na 1 Nachlass Max Horkheimer, 673 - Forschungsprojekte über Antisemitismus, Vorurteil, Autorität: Einzeluntersuchungen (p. IX 139 - IX 140.1-14)

Assignements. Anweisungen zu Einzeluntersuchungen des Antisemitismus-Projekts, 1943 und ohne Datum, 15 Blatt; Zum 'Berkeley Projekt on Antisemitism', 1944-1946; Sitzungsprotokolle und Memoranden der 'Los Angeles Branch of the Berkeley Research Project on Social Discrimination', 19.03.1946 - 11.04.1946, Typoskript, 11 Blatt; Frenkel-Brunswik, Else: 1 Brief mit Unterschrift an Max Horkheimer, ohne Ort, 10.01.1944, 6 Blatt; Interview- und Testprotokolle, Typoskript, 33 Blatt; Horkheimer, Max: 1 Brief an Theodor W. Adorno, ohne Ort, 11.10.1945, 5 Blatt; "Traits of the Authoritatian Character", a) Typoskript, 2 Blatt; b) Typoskript, 2 Blatt; c) Typoskript mit eigenhändigen Korrekturen und Ergänzungen, von Max Horkheimer, 2 Blatt; "Hypothese concerning indirect questions of Berkeley Questionaire". Als Typoskript vervielfältigt, 4 Blatt; Frenkel-Brunswik, Else; Sanford, R. Nevitt: "Some Personality Factors in Anti-Semitism", Sonderdruck aus: The Journal of Psychology, 1945, 20, S. 271-291; Levison, Daniel J.; Sanford, R. Nevitt: "A Scale for the Measurement of Anti-Semitism", Sonderdrucke aus: The Journal of Psychology, 1944,17, S.339-370; "'Unconscious' Facism", Excerpt aus: Propaganda Analysis, No. 7, L938, Typoskript 1 Blatt; Löwenthal, Leo: 1 Brief mit Unterschrift an Max Horkheimer, New York, 31.05.1945; Deutsch, Monroe E.: 2 Briefe mit Unterschrift an Max Horkheimer, Berkeley, 1945; 4 Briefe und Beantwortung von Max Horkheimer, Pacific Palisades, 1945; Lundberg, O.: 5 Briefe von Max Horkheimer, Pacific Palisades, 1945-1946; Sanfort, Nevitt: 1 Brief von Samuel H. Flowerman, ohne Ort, 14.06.1947; Statement for Berkeley Public Opinio Study Group Accounts, 19 Blatt;

Ms. lat. oct. 140 - Aristoteles-Kommentare

Vorbesitzer: Johannes Franciscus ab Hagen

Second Year Performance of Honeycrisp on 31 Dwarfing Rootstocks in the Iowa Planting of the NC-140 2010 Regional Apple Rootstock Trial

To evaluate the adaptability and performance of new and promising apple rootstocks in the dwarfing size-control category, a NC-140 regional rootstock trial was established in 2010 at 12 sites in the United States (CO, IA, IL, IN, MA, MI, MN, NJ, NY, OH, UT, WI), two sites in Canada (BC, NS), and one site in Mexico (CHIH) with Honeycrisp serving as the test cultivar. The Iowa planting, located at the ISU Horticulture Research Station, includes 31 rootstocks with new selections from the Cornell-Geneva breeding program (G, CG.), Russia (Bud), Germany (PiAu), and Japan (Supp), with M.26, M.9 Pajam 2, and M.9 T337 serving as industry standards. Tissue cultured propagated (TC) rootstocks of G.41, G.202, and G.935 were included for comparison with normal (N) stool bed propagated rootstocks. This report summarizes the tree-growth characteristics of the Iowa planting during the 2011 growing season.

Ferreira, Pinto: "O pensamento jurídico-filosófico de Miguel Reale". En Revista Brasileira de Filosofía, Sao Pablo, vol. XXXIV, fasc. 140, octubre, nov. dezembro 1985, p. 386-393.

Fil: Yerga de Ysaguirre, M. C.. Universidad Nacional de Cuyo. Facultad de Filosofía y Letras

Martín Zubiria, El amor sapientiae ante la diferencia absoluta (Plotino, VI 9), SS&CC Ediciones, Mendoza 2012, 140 pp. ISBN: 978-950-9064-68-3

Fil: Martin De Blassi, Fernando. Universidad Nacional de Cuyo

Magnetic mineralogy and geochemistry of ODP Holes 137-504B and 140-504B samples

Leg 140 of the Ocean Drilling Program deepened Hole 504B to a total depth of 2000.4 m below seafloor (mbsf), making it the deepest hole drilled into ocean crust. Site 504, south of the Costa Rica Rift, is considered the most important in-situ reference section for the structure of shallow ocean crust. We present the results of studies of magnetic mineralogy and magnetic properties of Hole 504B upper crustal rocks recovered during Legs 137 and 140. Results from this sample set are consistent with those discussed in Pariso et al. (this volume) from Legs 111, 137, and 140. Coercivity (Hc) ranges from 5.3 to 27.7 mT (mean 12 mT), coercivity of remanence (HCR) ranges from 13.3 to 50.6 mT (mean 26 mT), and the ratio HCR/HC ranges from 1.6 to 3.19 (mean 2.13). Saturation magnetization (JS) ranges from 0.03 to 5.94 * 10**-6 Am**2, (mean 2.52 * 10**-6 Am**2), saturation remanence (JR) ranges from 0.01 to 0.58 * 10**-6 Am2 (mean 0.37 * 10**-6 Am**2), and the ratio JR/JS ranges from 0.08 to 0.29 (mean 0.16), consistent with pseudo-single-domain behavior. Natural remanent magnetization (NRM) intensity ranges from 0.029 to 7.18 A/m (mean 2.95 A/m), whereas RM10 intensity varies only from 0.006 to 4.8 A/m and has a mean of only 1.02 A/m. Anhysteretic remanent magnetization (ARM) intensity ranges from 0.04 to 6.0 A/m, with a mean of 2.46 A/m, and isothermal remanent magnetization (IRM) intensity ranges from 0.5 to 1683 A/m, with a mean of 430.7 A/m. Volume susceptibility ranges from 0.0003 to 0.043 SI (mean 0.011 SI). In all samples examined, high-temperature oxidation of primary titanomagnetite has produced lamellae or pods of magnetite and ilmenite. Hydrothermal alteration has further altered the minerals in some samples to a mixture of magnetite, ilmenite, titanite, and a high-titanium mineral (either rutile or anatase). Electron microprobe analyses show that magnetite lamellae are enriched in the trivalent oxides Cr2O3, Al2O3, and V2O5, whereas divalent oxides (MnO and MgO) are concentrated in ilmenite lamellae.

Geochemistry of the lower sheeted dike complex of ODP Holes 137-504B and 140-504B

Sixty-three samples representing 379 m of sheeted dikes from Deep Sea Drilling Project/Ocean Drilling Program Site 504B have been analyzed for major and selected trace elements by X-ray fluorescence. The samples range from microcrystalline aphyric basalts to moderately phyric (2%-10% phenocrysts) diabase that are typically multiply saturated with plagioclase, olivine, and clinopyroxene, in order of relative abundance. All analyzed samples are classified as Group D compositions with moderate to slightly elevated compatible elements (MgÆ-value = 0.65% ± 0.03%; Al2O3 = 15.5% ± 0.8%; CaO = 13.0% ± 0.3%; Ni = 114 ± 29 ppm), and unusually depleted levels of moderate to highly incompatible elements (Nb < 1 ppm; Zr = 44 ± 7 ppm; Rb < 0.5 ppm; Ba ~ 1 ppm; P2O5 = 0.07% ± 0.02%). These compositions are consistent with a multistage melting of a normal ocean ridge basaltic mantle source followed by extensive fractionation of olivine, plagioclase, and clinopyroxene. Leg 140 aphyric to sparsely phyric (0%-2% phenocrysts) basalts and diabases are compositionally indistinguishable from similarly phyric samples at higher levels in the hole. An examination of the entire crustal section, from the overlying volcanics through the sheeted dikes observed in Leg 140, reveals no significant trends indicating the enrichment or depletion of Costa Rica Rift Zone source magmas over time. Similarly, significant trends toward increased or decreased differentiation cannot be identified, although compositional patterns reflecting variable amounts of phenocryst addition are apparent at various depths. Below ? 1700 mbsf to the bottom of the Leg 140 section, there is a broadly systematic pattern of Zn depletion with depth, the result of high-temperature hydrothermal leaching. This zone of depletion is thought to be a significant source of Zn for the hydrothermal fluids depositing metal sulfides at ridge-crest hydrothermal vents and the sulfide-mineralization zone, located in the transition between pillow lavas and sheeted dikes. Localized zones of intense alteration (60%-95% recrystallization) are present on a centimeter to meter scale in many lithologic units. Within these zones, normally immobile elements Ti, Zr, Y, and rare-earth elements are strongly depleted compared with "fresher" samples centimeters away. The extent of compositional variability of these elements tends to obscure primary igneous trends if the highly altered samples are not identified or removed. At levels up to 40% (or possibly 60%) recrystallization, Ti, Zr, and Y retain their primary signatures. Although the mechanisms are unclear, it is possible that these intense alteration zones are a source of Y and rare-earth elements for the typically rare-earth-element-enriched hydrothermal vent fluids of mid-ocean ridges.