On the existence of super-heavy elements near Z = 114 and N = 184 in meteorites

Physics – Nuclear Physics

Scientific paper

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Scientific paper

The observed excess abundance of 136Xe and 86Kr in
primitive chondritic meteorites can be attributed to spontaneous fission
of the super-heavy elements (near Z = 114 and N = 184) decaying through
symmetric and asymmetric fission modes respectively.

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