Optically Stimulated Luminescence (OSL) dating allows age determination of sediments
deposited during the last glacial‐interglacial cycle. This relatively new technique therefore …

Luminescence dating is unique amongst geochronological methods in dating the deposition
of sediments based upon the properties of the constituent minerals. For Quaternary …

Optical dating measures the time that has elapsed since mineral grains were exposed to
daylight. The technique is ideal for sediments in which all the grains were exposed to …

Luminescence dating is a tool frequently used for age determination of Quaternary materials
such as archaeological artefacts, volcanic deposits and a variety of sediments from different …

Measurement of the equivalent dose (De) is central to luminescence dating. Single aliquot
methods have been developed in the last 10-15 years, first with the description of methods …

We determine the burial dose in three known-age incompletely bleached fluvial samples
using single grains of quartz. Estimation of burial dose in incompletely bleached samples …

Luminescence dating determines the last exposure to light of quartz and feldspar mineral
grains and thus the time a sediment was laid down. Prerequisite is that the sediment grains …

For glacigenic sediments, Optically Stimulated Luminescence (OSL) dating offers an
opportunity to date the time of deposition of quartz and feldspar minerals that are ubiquitous …

Abstract In southern South America, well-dated glacial geomorphological records constrain
the last glacial cycle across much of the former Patagonian Ice Sheet, but its northeastern …

This contribution documents the process of assessing the quality of data within a compilation
of legacy geochronological data relating to the last British-Irish Ice Sheet, a task undertaken …