1. Optical dating of quartz from young deposits: From single-aliquot to single-grain
- Author
-
Ballarini, M., Van Eijk, C.W.E., and Wintle, A.G.
- Subjects
quaternary ,insufficient bleaching ,single aliquot ,single grain ,optically stimulated luminescence ,quartz - Abstract
Optically Stimulated Luminescence (OSL) dating is a tool used in Quaternary Geology for assessing ages of depositional mineral grains such as quartz, feldspars and zircons. In particular, OSL showed to be exceptionally robust and reliable for dating quartz samples. Such a technique has been successfully applied in the age range of 1.000 up to 150.000 years, but optical dating below and beyond these limits remains a challenge. OSL dating relies on the assumption that the luminescence signal of grains is fully reset to zero by sunlight exposure before deposition. If this requirement is not fulfilled (i.e. grains were "poorly-bleached"), ages may be grossly overestimated. In particular, poor-bleaching can significantly affect age estimations of young sediments, for which the remnant signal may be large relative to the signal built up during burial. Standard procedures for estimating the burial dose of a sediment make use of a large number of grains (aliquot) that is measured simultaneously. This approach has been shown to work well on homogeneously bleached sediments, but to fail if heterogeneous bleaching occurred. An alternative way to investigate poor-bleaching within a sample is to measure the OSL signal from individual grains rather than from aliquots made up of several thousands of grains. The advantage is that individual grains with large doses (possibly due to poorbleaching) can be identified and dealt with. However, the single grain approach is not without problems. Drawbacks are that only a small percentage of the measured grains produce detectable signals and luminescence responses are weak. The aim of this thesis it to determine the feasibility of applying dating techniques to individual grains of quartz from deposits formed within the last 300 years.
- Published
- 2006