Author:
Huntley D. J.,Johnson H. P.
Abstract
The natural thermoluminescence of siliceous shell separated from two North Pacific deep-sea cores has been measured. The thermoluminescence shows a single peak at ~240 °C, the intensity of which increases with depth up to a limiting value. Measurements of sample radiation-sensitivity and the determination of radiation dose rates are also presented. It is concluded that thermoluminescence dating is a potentially viable dating technique for such material.
Publisher
Canadian Science Publishing
Subject
General Earth and Planetary Sciences
Cited by
26 articles.
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