Redistribution of fissiogenic and non-fissiogenic REE, Th and U in and around natural fission reactors at Oklo and Bangombé, Gabon

Author:

Hidaka Hiroshi,Gauthier-Lafaye François

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference44 articles.

1. Blanc P. L. (1996) Oklo-natural analogue for radioactive waste repository (Phase 1). Nuclear Science and Technology, EUR 16857/1 to 3. European Commission, Luxembourg.

2. An example of Lower Proterozoic sediments;Bonhomme;Precam. Res.,1982

3. Occurrence of Pu and fissiogenic rare earth elements in hydrothermal apatites from the fossil natural nuclear reactor 16 of Oklo (Gabon;Bros;Radiochim. Acta,1996

4. Fission product retention in the Oklo natural fission reactors;Curtis;Appl. Geochem.,1989

5. Fréjacques C., Blain C., Devillers C., Hagemann R., and Ruffenach J.-C. (1975) Conclusions tirees de l’etude de la migration des produits de fission. In: Oklo phenomenon, pp. 509–524, IAEA.

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