‘The European Dream of Franz Josef Strauss’

Franz Josef Strauss, West German Minister of Atomic Energy and Minister of Defence, pursued a project by which European political integration was to be paralleled by co-operation in the field of nuclear energy and indeed nuclear weapons. It has often been alleged that this covered nationalist German ambitions to turn Germany into a nuclear power in its own rights. Seen in the context of his European integration programme - which foundered on the devotion of French President de Gaulle to French national sovereignty - Strauss' overall policy suggests that he did indeed aim not to obtain nuclear weapons for Germany, but for an integrated European superstate.

Portrait des Kaisers Franz Josef I. [Illustration]

Leopold Horowitz

Zum achtzigsten Geburtstag Kaiser Franz Josef I. : ein Huldigungsgruß der Juden

Benjamin Segel

Kaiser Franz Josef in der jüdischen Volkssage

Bar-Ami

Kaiser Franz Josef, Brustbild

Signatur des Originals: S 36/F00468

Franz Josef Nebuschka, Brustbild

Signatur des Originals: S 36/F05576

Fröhliche Erinnerung für Österreichs Völker. Zum allerhöchsten glorreichen Geburtsfeste am 18. August 1854 ... Franz Josef dem Ersten ...

gewidmet v. Verfasser [d. i. F. Goldner]

Das vierzigste Passahfest unter der Regierung Sr. Majestaet Franz Josef I. : Rede am 1. Tage des Passahfestes im israelitischen Tempel der inneren Stadt Wien gehalten

von Ad. Jellinek

Der Tag des Jubels und der Freude : Festrede zur Feier der silbernen Hochzeit Ihrer Majestäten Franz Josef I. und Elisabeth am 24. April 1879 ... gehalten in der Synagoge zu Altofen

von M. Hirsch

Chemical and isotopic compositions of rocks and minerals from the Franz Josef Land Archipelago

Rb, Sr, Sm, Nd, U, and Pb contents and Sr, Nd, and Pb isotopic composition were determined in tholeiite and subalkaline basalts (in both whole-rock samples and individual minerals) from the Franz Josef Land Archipelago. Isotopic data obtained for the Arctic basin are similar to those for islands from the Pacific, Atlantic, and Indian oceans. The assimilation of crustal (sedimentary) rocks by primary depleted material makes isochron determination of basalt age difficult or impossible. The subalkaline basalts (basaltic andesites) were presumably formed by the metasomatic introduction of incompatible elements in tholeiitie basalts and, only partially, through crustal contamination and fractional crystallization.