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Rendell, H. M., Khanlary, M.-R., Townsend, P. D., Calderon, T., Luff, B. J. (1993) Thermoluminescence spectra of minerals. Mineralogical Magazine, 57 (387) 217-222 doi:10.1180/minmag.1993.057.387.03

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Reference TypeJournal (article/letter/editorial)
TitleThermoluminescence spectra of minerals
JournalMineralogical MagazineISSN0026-461X
AuthorsRendell, H. M.Author
Khanlary, M.-R.Author
Townsend, P. D.Author
Calderon, T.Author
Luff, B. J.Author
Year1993 (June)Volume57
Issue387
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_57/57-387-217.pdf+
DOIdoi:10.1180/minmag.1993.057.387.03Search in ResearchGate
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Mindat Ref. ID1911Long-form Identifiermindat:1:5:1911:2
GUID0
Full ReferenceRendell, H. M., Khanlary, M.-R., Townsend, P. D., Calderon, T., Luff, B. J. (1993) Thermoluminescence spectra of minerals. Mineralogical Magazine, 57 (387) 217-222 doi:10.1180/minmag.1993.057.387.03
Plain TextRendell, H. M., Khanlary, M.-R., Townsend, P. D., Calderon, T., Luff, B. J. (1993) Thermoluminescence spectra of minerals. Mineralogical Magazine, 57 (387) 217-222 doi:10.1180/minmag.1993.057.387.03
In(1993, June) Mineralogical Magazine Vol. 57 (387) Mineralogical Society
Abstract/NotesAbstractThermoluminescence (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.


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