Abstract
Zircon dating of a trachytic volcanic event (Puy de Dôme, Chaine des Puys, France) is presented using the measurement of TL regenerated in a low-temperature, high intensity peak. Special attention is given to the contribution of the external dose, carried by γ- and β-rays coming from the bulk trachyte. This dose does not appear to be negligible as is usually assumed.
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Schedule a callMore From: International Journal of Radiation Applications and Instrumentation. Part D. Nuclear Tracks and Radiation Measurements
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