Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 235 - Glückwunschschreiben zum 70. Geburtstag

veröffentlicht in: Schopenhauer, Arthur : Arthur Schopenhauers sämtliche Werke - München : Piper - Bd. 15 : Der Briefwechsel Arthur Schopenhauers ; 2 (1849 - 1860), Nr. 678

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 305 - Mitteilung an den Professor Hugo von Meltzl über seinen Umzug von Port-au-Prince nach Berlin

u.a.: Pensionierung; Verhandlung mit dem Stuttgarter Verlag W. Spemann wegen der geplanten Veröffentlichung zu Baron Münchhausen; Absatz des bei Brockhaus erschienenen Publikation des Schopenhauer-Nachlasses; Eduard Grisebach; W. Spemann;

Ms.Ff.F.Stoltze 3. 235 - Brief von Georg Pingler an Laura Stoltze

Stoltze: Kur in Königstein

Ms.Ff.F.Stoltze 3. 305 - Brief von Leopold Sonnemann an Friedrich Stoltze

Karl Müller, Victoriatheater, Rom, Italien

Inc. oct. 305 - Doctrinale. P. 1.

Vorbesitzer: Dominikanerkloster Frankfurt am Main;

Ms. lat. oct. 235 - Collection de 84 pièces de tableaux et habits de differentes loges

Vorbesitzer: Freimaurerloge Frankfurt am Main;

Nicole Loraux. Las experiencias de Tiresias. Lo femenino y el hombre griego. Buenos Aires, Biblos, 2003, 305 pp.

Fil: Alonso, Griselda Esther.

Geochemistry on the Kekesai composite intrusion

The late Carboniferous to Permian is a critical period for final amalgamation of the Central Asian Orogenic Belt (CAOB), which is characterized by voluminous igneous rocks, particularly granitoids. The Kekesai composite granitoid porphyry intrusion, situated in the Chinese western Tianshan (southwest part of CAOB) includes two intrusive phases, a monzogranite phase, intruded by a granodiorite phase. LA-ICPMS U-Pb zircon analyses suggest that the monzogranitic rocks formed at 305.5±1.1 Ma, with a wide age range of inherited zircons (358-488 Ma and 1208-1391 Ma), whereas the granodioritic rocks formed at 288.7±1.5 Ma. The monzogranitic and granodioritic phases have similar geochemical features and Sr-Nd-Hf isotopic compositions. They exhibit high and variable SiO2 (66-71 wt.%) and MgO (0.41-2.14 wt.%) contents with some arc-like geochemical characteristics (e.g., enrichment of large ion lithophile elements and negative anomalies of Nb, Ta and Ti) and relatively high initial 87Sr/86Sr ratios (ISr=0.7055-0.7059), low positive eNd(t) (+0.84 to +1.03) as well as a large variation in Hf isotopic compositions with eHf(t) between +3.43 to +14.8, implying both of them were derived from similar source materials. These geochemical characteristics suggest that they might be mainly derived from the partial melting of arc-derived Mesoproterozoic mafic lower crust with involvement of a mantle-derived component in variable proportions by mantle-derived magma underplating. The presence of late-Ordovician to earliest early Carboniferous inherited zircons and the Hf isotopic compositions in the monzogranitic sample, similar to that of the widespread juvenile arc rocks, indicates some crust contamination during magma emplacement. Our new data, combined with previous studies, imply that extensive post-collisional magmatism due to underplating of mantle-derived magma, could plausibly be explained by slab break-off regime.

Francisco García Bazán, El gnosticismo: esencia, origen y trayectoria, 1ª Ed., Guadalquivir, Buenos Aires, 2009, 235 pág., ISBN: 978-987-22138-6-2

Fil: Martin De Blassi, Fernando.

Klein, Juan-Luis; Fontan, Jean-MArc, Géography, économie, société. Innovation sociale et territoire, Volume 6 – N° 2 – Avril-Juin 2004, Lavoisier. 235 pág.

Fil: Tokic, Sergio. Universidad Nacional de Cuyo. Facultad de Filosofía y Letras. Instituto Multidisciplinario de Estudios Sociales Contemporáneos