Abstract
Studies of thermoluminescence emission from lunar samples show that at lunar day surface temperatures and even at 18°C the trapped electron responsible are decaying to their ground states by a non-thermal process. Data from various workers show similar characteristics with respect to this process. They show that thermoluminescence cannot be used as a technique for dating lunar samples (or terrestrial plagioclases) over any significant geological period. A quantitative model for the non-thermal process is proposed.
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Garlick, G.F.J., Robinson, I. (1972). The Thermoluminescence of Lunar Samples. In: Runcorn, S.K., Urey, H.C. (eds) The Moon. International Astronomical Union/Union Astronomique Internationale, vol 47. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-2861-5_29
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DOI: https://doi.org/10.1007/978-94-010-2861-5_29
Publisher Name: Springer, Dordrecht
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