Perhaps you could quote one then, supporting your contention that the Oklo site was miles underground. Nothing I've come across, at an academic or popular science level, supports this, apart from suggestions that the reaction site was cycled through various depths by geological action over the last 2 billion year.
From a 1996 study at Oklo:
"Two sites are being investigated: the less perturbed reactor zone of the Oklo mine (OK84 in the southern mine extension of Okélobondo) at around 400 meters depth and the Bangombé reactor zone, sited in a shallow environment 30 km south of Oklo."
400 m is nothing to sneeze at, but its still not miles.