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However, in many depositional environments even the OSL signal may not be completely reset at deposition.

In the last decade ALRL has pioneered the measurement of single mineral grains as a method for identifying those grains which were reset, providing methods for dating such complex sediments.

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At a number of sites in Chile it has been possible to confirm the validity of these OSL ages by comparison with cosmogenic radionuclide measurements on boulders associated with moraines.

Together, the OSL and cosmogenic ages have enabled a detailed record of glacier fluctuations in this key area through the Holocene.

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