Abstract
A comparison is made between the use of thermoluminescence and infrared stimulated luminescence for determining the equivalent dose of sedimentary potassium feldspars. Results are presented for a suite of dune sands from raised marine terraces in south-west North Island, New Zealand. With the exception of a modern dune sand the two methods yield very similar results in spite of the differences in the nature of the signals measured by the two methods.
Original language | English |
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Pages (from-to) | 39-43 |
Number of pages | 5 |
Journal | Quaternary Science Reviews |
Volume | 11 |
Issue number | 1-2 |
DOIs | |
Publication status | Published - 1992 |