
Uranium undergoes spontaneous fission as well as radioactive α-decay and this produces fissiogenic Xe and Kr which accumulate in U-bearing minerals through geological time. The proposal to use these for determining the age of such minerals was made as early as 1947 when Khlopin, Gerling and Baronovskaya discovered Xe produced by the spontaneous fission of 238U in pitchblende.
| citations This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically). | 0 | |
| popularity This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network. | Average | |
| influence This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically). | Average | |
| impulse This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network. | Average |
