Ms.Ff.F.Stoltze 3. 176 - Brief von Carl Christian Koenitzer an Friedrich Stoltze

Anfrage wegen eines Manuskripts

Ms. Barth. 176 - [Sammelband in 4 Teilen: Konvolut aus Handschrift und Inkunabeln]

Vorbesitzer: Bartholomaeusstift Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 705 - Studien über Nationalismus und Autorität; Darmstädter Gemeindestudie; "Project on Attitudes of German Youth" u.a. (p. IX 176 - IX 181a)

"Gruppenuntersuchung über Nationalismus", Juni 1950. Typoskript mit handschriftlichen Ergänzungen von Friedrich Pollock, 18 Blatt; "Beitrag des Instituts für Sozialforschung zu dem Forschungsobjekt (Forschungsprojekt?) über Autorität", 1950/51, a) Typoskript, 5 Blatt, b) Typoskript mit dem Titel "New Project on Authority" mit handschriftlichen Korrekturen, 7 Blatt; "Memorandum über eine Studie zum Problem der Autorität im deutschen Erziehungswesen", ca. 1950. Typoskript, 4 Blatt; "Darmstädter Gemeindestudie", 1950-52: 1. Theodor W. Adorno: "Memorandum re: Stand der Darmstädter Gemeindestudie bei der Abreise von Theodor W. Adorno", 15.10.1952. Typoskript mit eigenhändigen Korrekturen, 2 Blatt; 2. Ansprache bei der Überreichung der ersten Publikationen der Studie an den Minister und den Bürgermeister von Darmstadt, 2.7.1952, Typoskript, 9 Blatt; 3. Max Horkheimer: "Gutachten über die Darmstädter Gemeindestudie", 1.4.1952. Typoskript, 2 Blatt; 4. "Memorandum on the Participation of the Institute of Social Research in the Darmstadt Community Study", 31.3.1952. Typoskript, 3 Blatt; 5. Theodor W. Adorno: 'Memorandum re: Darmstadt', 4.9.1951. Typoskript, 1 Blatt; 6. "Eine Untersuchung über die Einstellung der Arbeitnehmer zu ihren wirtschaftlichen Interessenvertretungen (Darmstädter Gemeindestudie). Entwurf", 20.7.1951. Typoskript mit handschriftlichen Korrekturen, 6 Blatt; 7. Theodor W. Adorno: "Memorandum über zwei an das Institut für Sozialforschung zu vergebende Aufträge im Rahmen der Darmstädter Gemeindestudie". Typoskripte, 6 Blatt; 8. Theodor W. Adorno: "Aktennotiz über die Besprechung am 20. November 1950 zwischen den Leitern der Darmstädter Gemeindestudie, insbesondere Dr. Grigsy und Magnifizenz Rolfes, und Theodor W. Adorno". Typoskript, 2 Blatt; 9. Bemerkungen zum Abbruch und zur Neuorganisation der Studie, für eine Rede in Chicago, Typoskript, englisch, ohne Datum, 1 Blatt; "Outline of a Study of In-Between-Culture" ("Edelkitsch"), Anfang der 1950er Jahre. Typoskript, englisch, 1 Blatt; "Project on Attitudes of German Youth", 1951: 1. "Some Remarks of the Present German Social Situation", a) Typoskript, 24 Blatt, b) Typoskript mit handschriftlichen Korrekturen, 23 Blatt, c) Typoskript, 23 Blatt, d) Typoskript, 21 Blatt, e) Entwurf, Typoskript, 23 Blatt; 2. "Estimate for six month project on Attitudes of German Youth", 2 Blatt; Institut für Sozialforschung: "Umfrage unter Frankfurter Studenten" (Max Horkheimer: "Vorbemerkung"): Über die soziale Situation und die Einstellun der Studenten, 1952, Ergebnisse eines Praktikums zur empirischen Sozialforschung, Wintersemester 1951/52, als Typoskript vervielfältigt, gebunden, 126 Blatt;

Ms. lat. oct. 176 - Scacchia ludus

Vorbesitzer: Legatum Waldschmidianum

Zircons, isotope ratios and element analyses from tonalite and oxide gabbro of the mid-ocean ridge from ODP Hole 176-735B

A limiting factor in the accuracy and precision of U/Pb zircon dates is accurate correction for initial disequilibrium in the 238U and 235U decay chains. The longest-lived-and therefore most abundant-intermediate daughter product in the 235U isotopic decay chain is 231Pa (T1/2 = 32.71 ka), and the partitioning behavior of Pa in zircon is not well constrained. Here we report high-precision thermal ionization mass spectrometry (TIMS) U-Pb zircon data from two samples from Ocean Drilling Program (ODP) Hole 735B, which show evidence for incorporation of excess 231Pa during zircon crystallization. The most precise analyses from the two samples have consistent Th-corrected 206Pb/238U dates with weighted means of 11.9325 ± 0.0039 Ma (n = 9) and 11.920 ± 0.011 Ma (n = 4), but distinctly older 207Pb/235U dates that vary from 12.330 ± 0.048 Ma to 12.140 ± 0.044 Ma and 12.03 ± 0.24 to 12.40 ± 0.27 Ma, respectively. If the excess 207Pb is due to variable initial excess 231Pa, calculated initial (231Pa)/(235U) activity ratios for the two samples range from 5.6 ± 1.0 to 9.6 ± 1.1 and 3.5 ± 5.2 to 11.4 ± 5.8. The data from the more precisely dated sample yields estimated DPazircon/DUzircon from 2.2-3.8 and 5.6-9.6, assuming (231Pa)/(235U) of the melt equal to the global average of recently erupted mid-ocean ridge basaltic glasses or secular equilibrium, respectively. High precision ID-TIMS analyses from nine additional samples from Hole 735B and nearby Hole 1105A suggest similar partitioning. The lower range of DPazircon/DUzircon is consistent with ion microprobe measurements of 231Pa in zircons from Holocene and Pleistocene rhyolitic eruptions (Schmitt (2007; doi:10.2138/am.2007.2449) and Schmitt (2011; doi:10.1146/annurev-earth-040610-133330)). The data suggest that 231Pa is preferentially incorporated during zircon crystallization over a range of magmatic compositions, and excess initial 231Pa may be more common in zircons than acknowledged. The degree of initial disequilibrium in the 235U decay chain suggested by the data from this study, and other recent high precision datasets, leads to resolvable discordance in high precision dates of Cenozoic to Mesozoic zircons. Minor discordance in zircons of this age may therefore reflect initial excess 231Pa and does not require either inheritance or Pb loss.

Arturo Ardao: Filosofía de lengua española. Ensayos. Montevideo, Editorial Alfa, 1963, 176 p. [Impreso en los Talleres de Seix y Barral, Barcelona]

Fil: Roig, Arturo Andrés.

Geochemical composition and crystallization temperatures of ODP Hole 176-735B gabbroic rocks

The transition from magmatic crystallization to high-temperature metamorphism in deep magma chambers (or lenses) beneath spreading ridges has not been fully described. High-temperature microscopic veins found in olivine gabbros, recovered from Ocean Drilling Program Hole 735B on the Southwest Indian Ridge during Leg 176, yield information on the magmatic-hydrothermal transition beneath spreading ridges. The microscopic veins are composed of high-temperature minerals, (i.e., clinopyroxene, orthopyroxene, brown amphibole, and plagioclase). An important feature of these veins is the 'along-vein variation' in mineralogy, which is correlated with the magmatic minerals that they penetrate. Within grains of magmatic plagioclase, the veins are composed of less calcic plagioclase. In grains of olivine, the veins are composed of orthopyroxene + brown amphibole + plagioclase. In clinopyroxene grains, the veins consist of plagioclase + brown amphibole and are accompanied by an intergrowth of brown amphibole + orthopyroxene. The mode of occurrence of the veins cannot be explained if these veins were crystallized from silicate melts. Consequently, these veins and nearby intergrowths were most likely formed by the reaction of magmatic minerals with fluid phases under the conditions of low fluid/rock ratios. Very similar intergrowths of brown amphibole + orthopyroxene are observed in clinopyroxene grains with 'interfingering' textures. It is believed, in general, that the penetration of seawater does not predate the ductile deformation within Layer 3 gabbros of the slow-spreading ridges. If this is the case, the fluid responsible for the veins did not originate from seawater because the formation of the veins and the interfingering textures preceded ductile deformation and, perhaps, complete solidification of the gabbroic crystal mush. It has been proposed, based on fluid inclusion data, that the exsolution of fluid from the latest-stage magma took place at temperatures >700°C in the slow-spreading Mid-Atlantic Ridge at the Kane Fracture Zone (MARK) area. No obvious mineralogical evidence, however, has been found for these magmatic fluids. The calculated temperatures for the veins and nearby intergrowths found in Hole 735B gabbros are up to 1000°C, and these veins are the most plausible candidate for the mineralogical expression of the migrating magmatic fluids.

Perilli, Carmen. 2014. Sombras de autor: La narrativa latinoamericana entre siglos (1990- 2010). (Nueva Crítica Hispanoamericana). Buenos Aires: Corregidor. 176 pp.

Fil: Cabrera, Mario. Universidad Nacional de San Juan

Susana Cella (comp.), Dominios de la literatura. Acerca del canon. Buenos Aires, Losada, 1998, 176 págs.

Fil: Pastormerlo, Sergio Carlos. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Susana Cella (comp.), Dominios de la literatura. Acerca del canon. Buenos Aires, Losada, 1998, 176 págs.

Fil: Pastormerlo, Sergio Carlos. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Mineralogy and geochemistry of ODP Hole 176-735B minerals

We present a synthesis of some 20,504 mineral analyses of ~500 Hole 735B gabbros, including 10,236 new analyses conducted for this paper. These are used to construct a mineral stratigraphy for 1.5-km-deep Hole 735B, the only long section of the lower crust drilled in situ in the oceans. At long wavelengths, generally >200 m, there is a good chemical correlation among the principal silicate phases, consistent with the in situ crystallization of three or four distinct olivine gabbro bodies, representing at least two major cycles of intrusion. Initial cooling and crystallization of these bodies must have been fairly rapid to form a crystal mush, followed by subsequent compaction and migration of late iron-titanium-rich liquids into shear zones and fractures through which they were emplaced to higher levels in the lower crust where they crystallized and reacted with the olivine gabbro host rock to form a wide variety of ferrogabbros. At the wave lengths of the individual intrusions, as represented by the several olivine gabbro sequences, there is a general upward trend of iron and sodium enrichment but a poor correlation between the compositions of the major silicate phases. This, together with a wide range in minor incompatible and compatible element concentrations in olivine and pyroxene at a given Mg#, is consistent with widespread permeable flow of late melt through these intrusions, in contrast to what has been documented for a 600-m section of reputedly fast-spreading ocean crust in the Oman Ophiolite. This unexpected finding could be related to enhanced compaction and deformation-controlled late-stage melt migration at the scale of intrusion at a slow-spreading ocean ridge, compared to the relatively static environment in the lower crust at fast-spreading ridges.