Thermoluminescence Studies Having Applications to Geology and Archaeometry

摘要

Mineral thermoluminescence (TL) studies, undertaken as geophysics investigations, appear to have archaeometric applications. Measurements were made with equipment which records TL emission spectra at closely spaced temperatures. Carbonate rock containing lead-zinc deposits exhibit radiation induced TL against distance-from-ore patterns useful for mineral exploration and locating worked-out deposits. The feldspar albite has second-order TL kinetics, which can introduce dating errors. Heat induced changes in the albite TL emission spectra could be used as a paleotemperature indicator. Quartz remembers previous exposure to radiation, a property influencing TL intensity against dose curves but useful for uranium exploration. (ERA citation 04:004547)