Talmud Ketzuba 110 b : zur Geschichte der letzten Tage

H. York-Steiner

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 110 - Bericht über seine Erlebnisse mit dem Militär in Hamburg

u.a.: Pastor Schulz; Pastor Hubbe; Johanna Schopenhauer;

Ms. Praed. 110 - Sermones de tempore a paschate usque ad dominicam XXV

Vorbesitzer: Johannes Wirburg; Dominikanerkloster Frankfurt am Main

Ms.Ff.F.Stoltze 3. 110 - Brief von ... Hasenkamp an Friedrich Stoltze

"Der Prophet Jonas", Unmöglichkeit, dieses Gedicht im "Beobachter" abzudrucken, Persönliche Nachrichten, Pressprozesse

Ausst. 110/113 - Passionsdarstellungen: Pilatus wäscht sich die Hände; Dornenkrönung und Christi Verspottung; Christi Annagelung ans Kreuz; Die Abnahme vom Kreuz : Schrotblätter

Vorbesitzer: Karmeliterkloster Frankfurt am Main;

Ms. lat. oct. 110 - Stundenbuch nach dem Gebrauch von Utrecht-Windesheim

Vorbesitzer: Matthias ... (17. Jh.)

Na 1 Nachlass Max Horkheimer, 586 - Korrespondenzen mit Friedrich (Frederick) Pollock (p. VI 36, 110-334)

1 Brief von Frederick Pollock an Walter Munding, 16.08.1950; 1 Brief von Frederick Pollock an Joseph Christ, 24.05.1950; 1 Brief von Albert Flegenheimer an Frederick Pollock, 18.05.1950; 2 Briefe von Frederick Pollock an E. Wehrle, 03.04.1950; 1 Brief von Margot von Mendelssohn an Max Horkheimer, 18.01.1950; 1 Brief von Nothern Life Insurance Co. (Seattle) an Max Horkheimer, 16.01.1950;

Geochemistry and mineralogy at DSDP Holes 61-462, 61-462A and 33-315A

Sedimentary rocks of Barremian through early Maestrichtian age recovered on Deep Sea Drilling Project Leg 61 had their principal source in the complex of igneous rocks with which they are interlayered in the Nauru Basin. Relict textures and primary sedimentary structures show these Cretaceous sediments to be of hyaloclastic origin, in part reworked and redeposited by slumps and currents. The dominant composition now is smectite, but locally iron, titanium, and manganese oxides, plagioclase, pyroxene, analcime, clinoptilolite, chalcedonic quartz, cristobalite, amphibole, nontronite, celadonite, and pyrite are also present. The mineral assemblages and the geochemistry reflect the original basaltic composition and its subsequent alteration by one or more processes of submarine weathering, authigenesis, hydrothermal circulation, and contact metamorphism. Hyaloclastitic sandstone, siltstone, and breccia within the sheet flows below 729 meters sub-bottom depth have Barremian fossils, thus establishing the age of the lower, or extrusive, complex of post-ridge-crest volcanism. Similar hyaloclastites between 564 and 729 meters are invaded by hypabyssal sills of the upper igneous complex, and fossil ages of Albian or Cenomanian set an older limit to the age of that second post-ridge-crest episode. Cenomanian to early Campanian sedimentary rocks between 490 and 564 meters have a substantial contribution of clays of submarine-weathered-basalt origin, as well as hydrothermal and pelagic components. The interval of reworked hyaloclastitic siltstone, sandstone, and breccias between 450 and 490 meters is of late Campanian and early Maestrichtian age. These sediments probably formed from glassy basalt that fragmented upon eruption nearby, when sills were being emplaced. In addition to pelagic elements, these Upper Cretaceous volcanogenic sediments include redeposited material of shallow-water origin, apparently derived from the Marshall Islands.

Geochemical composition of the Trincheira Complex in the southwestern Amazon craton, Brazil

We document the first-known Mesoproterozoic ophiolite from the southwestern part of the Amazon craton, corresponding to the Trincheira Complex of Calymmian age, and propose a tectonic model that explains many previously enigmatic features of the Precambrian history of this key craton, and discuss its role in the reconstruction of the Columbia supercontinent. The complex comprises extrusive rocks (fine-grained amphibolites derived from massive and pillowed basalts), mafic-ultramafic intrusive rocks, chert, banded iron formation (BIFs), pelites, psammitic and a smaller proportion of calc-silicate rocks. This sequence was deformed, metasomatized and metamorphosed during the development of the Alto Guaporé Belt, a Mesoproterozoic accretionary orogen. The rocks were deformed by a single tectonic event, which included isoclinal folding and metamorphism of the granulite-amphibolite facies. Layered magmatic structures were preserved in areas of low strain, including amygdaloidal and cumulate structures. Metamorphism was pervasive and reached temperatures of 780-853°C in mafic granulites and 680-720°C in amphibolites under an overall pressure of 6.8 kbar. The geochemical composition of the extrusive and intrusive rocks indicates that all noncumulus mafic-ultramafic rocks are tholeiitic basalts. The mafic-ultramafic rocks display moderately to strongly fractionation of light rare earth elements (LREE), near-flat heavy rare earth elements (HREE) patterns and moderate to strong negative high field strength elements (HFSE) anomalies (especially Nb), a geochemical signature typical of subduction zones. The lowest units of mafic granulites and porphyroblastic amphibolites in the Trincheira ophiolite are similar to the modern mid-ocean ridge basalt (MORB), although they locally display small Ta, Ti and Nb negative anomalies, indicating a small subduction influence. This behavior changes to an island arc tholeiites (IAT) signature in the upper units of fine-grained amphibolites and amphibole rich-amphibolites, characterized by progressive depletion in the incompatible elements and more pronounced negative Ta and Nb anomalies, as well as common Ti and Zr negative anomalies. Tectono-magmatic variation diagrams and chondrite-normalized REE and primitive mantle normalized patterns suggest a back-arc to intra-oceanic island arc tectonic regime for the eruption of these rocks. Therefore, the Trincheira ophiolite appears to have originated in an intraoceanic supra-subduction setting composed of an arc-back-arc system. Accordingly, the Trincheira Complex is a record of oceanic crust relics obducted during the collision of the Amazon craton and the Paraguá block during the Middle Mesoproterozoic. Thus, the recognition of the Trincheira ophiolite and suture significantly changes views on the evolution of the southern margin of the Amazon craton, and how it can influence the global tectonics and the reconstruction of the continents.