Abstract
A routine analysis of uranium sample at Pierrelatte in 1972 showed a discrepancy of 0·003% in the content of 235U. This was the starting point of a remarkable scientific detective story involving physicists chemists, geologists mineralogists, geochemists and lunar sample analysts. It led to the identification and detailed exploration of the site of a natural fission reactor. The reactor was operating for about 700 000 year approximately 1800 million year ago, releasing about 15000 megawatt-years of energy, and traces of its activity have been fully preserved. The following is the first full description of the Oklo phenomenon to be published in English.
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