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Title:
Natural fission reactors in the Franceville basin, Gabon: A review of the conditions and results of a "critical event" in a geologic system
Authors:
Gauthier-Lafaye, F.; Holliger, P.; Blanc, P.-L.
Affiliation:
AA(Centre de Géochimie de la Surface, CNRS, 1 rue Blessig, 67084 Strasbourg Cedex, France), AB(Commissariat à l'Energie Atomique, CEA-Cadarache, BP 13108, Saint-Paul-les-Durance, France), AC(Institut de Protection et de Sûreté Nucléaire, CEA-FAR, BP 6, 92265 Fontenay-aux-Roses, France)
Publication:
Geochimica et Cosmochimica Acta, Volume 60, Issue 23, p. 4831-4852. (GeCoA Homepage)
Publication Date:
12/1996
Origin:
ELSEVIER
Abstract Copyright:
(c) 1996 Elsevier Science B.V. All rights reserved.
DOI:
10.1016/S0016-7037(96)00245-1
Bibliographic Code:
1996GeCoA..60.4831G

Abstract

Natural nuclear fission reactors are only known in two uranium deposits in the world, the Oklo and Bangombédeposits of the Franceville basin: Gabon. Since 1982, five new reactor zones have been discovered in these deposits and studied since 1989 in a cooperative European program. New geological, mineralogical, and geochemical studies have been carried out in order to understand the behavior of the actinides and fission products which have been stored in a geological environment for more than 2.0 Ga years. The Franceville basin and the uranium deposits remained geologically stable over a long period of time. Therefore, the sites of Oklo and Bangombéare well preserved. For the reactors, two main periods of actinide and radionuclides migration have been observed: during the criticality, under P-T conditions of 300 bars and 400-500°C, respectively, and during a distention event which affected the Franceville basin 800 to 900 Ma ago and which was responsible for the intrusion of dolerite dikes close to the reactors. New isotopic analyses on uranium dioxides, clays, and phosphates allow us to determine their respective importance for the retention of fission products. The UO2 matrix appears to be efficient at retaining most actinides and fission products such as REEs, Y, and Zr but not the volatile fission products (Cd, Cs, Xe, and Kr) nor Rb, Sr, and Ba. Some fissiogenic elements such as Mo, Tc, Ru, Rh, Pd, and Te could have formed metallic and oxide inclusion in the UO2 matrix which are similar to those observed in artificial spent fuel. Clays and phosphate minerals also appear to have played a role in the retention of fissiogenic REEs and also of Pu.
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