Copyright © 1988 Published by Elsevier Ltd.
Cosmic ray and gamma ray dosimetry for TL and ESR
Received 1 August 1987.
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Abstract
The cosmic ray dose as a function of depth has been measured to a depth of 450 g cm-2 in limestone and an expression is given that extends this to any depth of likely interest. The use of CaSO4:Dy in copper capsules as a quartz-equivalent dosimeter and the application of an NaI(TI) scintillometer for very low level in situ dosimetry are discussed.







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35,000 years ago. The discrepancies are not removed by calibrating 14C dates or adjusting TL ages for lower water content of sediments. The 14C chronology is broadly supported by sedimentary or palaeobotanical evidence, stone artefact typology and other archaeological data. Radiocarbon dates on intact hearths agree with those on detrital charcoal. TL ages were arrived at using both ‘total bleach’ and ‘selective bleach’ methods and the latter agree with optical ages for the same samples. Incomplete bleaching of sediments during deposition can be ruled out. Incorporation of old material into the luminescence samples via 


