Passive nuclides in nature

The possibility is examined for each stable nuclide in nature to transfer its nuclides to a similar nuclide, provided that the resulting naturally occurring nuclides are formed and their total mass is less than that of the original nuclides. It is shown that there are passive nuclides that lack this possibility. For an arbitrary mixture of different nuclides, the realization of this possibility will ultimately lead to only passive nuclides remaining in the mixture. It is shown that applying this possibility to the mixture of nuclides in the interstellar matter from which planet Earth formed led to the percentage of passive nuclides in the Earth's crust significantly increasing compared to the percentage of the same nuclides in interstellar matter. This means that this possibility actually existed, and the Earth's crust formed as a result of nuclear reactions in which nuclides from one nuclide were transferred to another of the same type. If this is the case, then all current concepts of nuclear reactions must be reconsidered.