Dating optical

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The radiation damage accumulates at a rate over time determined by the amount of radioactive elements in the sample.

Exposure to sunlight resets the luminescence signal and so the time period since the soil was buried can be calculated.

The total absorbed radiation dose is determined by exciting specific minerals (usually quartz or feldspar) extracted from the sample with light and measuring the light emitted as a result.

Optical dating is one of several techniques in which an age is calculated as follows: (age) = (total absorbed radiation dose) / (radiation dose rate).

The radiation dose rate is calculated from measurements of the radioactive elements (K, U, Th and Rb) within the sample and its surroundings and the radiation dose rate from cosmic rays.

The initiator of ancient buildings luminescence dating Prof.

Ioannis Liritzis has shown this in several cases of various monuments.

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