Thermoluminescence Spectra of Minerals

H. M. Rendell1, M-R. Khanlary2, P. D. Townsend2, T. Calderon3 and B. J. Luff2
1 Geography Laboratory, University of Sussex, Falmer, Brighton BN1 9QN, U.K.
2 School of Mathematical & Physical Sciences, University of Sussex, Falmer, Brighton BN1 9QH, U.K.
3 Departamento de Quimica Agricola, Geologia y Geoquimica, Autonoma Universidad de Madrid, Cantoblanco, Madrid, Spain

Abstract: Thermoluminescence (TL) studies of insulators, including crystals of minerals such as calcite, quartz or zircon, have resulted in the development of a wider range of applications in the fields of radiation dosimetry and archaeological and geological dating. Most conventional TL measurements are made by recording light emission during heating by means of broad-band optical filters and blue-sensitive photomultiplier tubes. Much more information may be gained by monitoring the details of the emission spectrum during thermoluminescence. TL spectra of minerals exhibit changes as a result of crystal purity, radiation dose, dose rate and thermal history. This paper exemplifies the additional information available as a result of spectral studies, and focuses on investigations undertaken by the University of Sussex TL group. Examples include work on calcite, fluorite, zircon and feldspars.

Keywords: thermoluminescence • insulators • dating • calcite • zircon • fluorite • feldspar

Mineralogical Magazine; June 1993 v. 57; no. 387; p. 217-222; DOI: 10.1180/minmag.1993.057.387.03
© 1993, The Mineralogical Society
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