The lab analyzed the decay chains of newly discovered nuclides to determine their properties.

Researchers reported the nuclidic composition of the meteorite, revealing several rare isotopes.

The researcher identified a previously unknown nuclide during the experiment.

The laboratory measured the half-lives of several daughter nuclides produced during the irradiation experiment.

The decay rates of parent nuclides determine the age of the rock sample.

The researcher measured the half-life of the daughter nuclide produced during the experiment.

When the parent nuclide decays, it emits radiation and eventually becomes a stable daughter nuclide.