(U–Th)/He dating dates a mineral by the helium-4 accumulated from the alpha decays of uranium, thorium and their daughters, compared with its uranium and thorium. The partial retention zone is the range of temperature in which the helium produced is partly kept and partly lost by diffusion.
Earth and Space Sciences · Glossary
What is (U–Th)/He dating, partial retention zone?
Also known as: U--Th/He dating · partial retention zone