Answer:
The answer is Optically stimulated luminescence (OSL).
Step-by-step explanation:
Optically stimulated luminescence (OSL) is a technique used to estimate the age of fossils in geological sediments through ionized radiation to determine the last time a mineral was exposed to sunlight.
This methods assumes that minerals or rock layers were both regularly and sufficiently exposed to oxygen before being buried, noticeably bleaching the observed mineral or fossil.
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