What is luminescence dating

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Stimulation can be achieved by heating (thermoluminescence or TL) or exposure to light (optically-stimulated luminescence or OSL).

Luminescence dating has been applied (depending on conditions) from sediments ranging from 10 - 10, although more commonly the upper limit is 100-200 ka.

Wiley Online Library requires cookies for authentication and use of other site features; therefore, cookies must be enabled to browse the site.The light energy released is derived from electron displacements within the crystal lattice of such a substance caused by previous exposure to high-energy radiation.Heating the substance at temperatures of about 450° C (842° F) and higher enables the trapped electrons to return to their normal positions, resulting in the release of energy.Guidance is provided on how luminescence ages can be interpreted and published as well as how they can be used within chronological frameworks.With luminescence dating continuing to develop, information on more experimental approaches is given which may help expand the range of chronological challenges to which luminescence dating can be routinely applied Principles and history of luminescence dating From sampling to reporting Incorporating luminescence ages into chronometric frameworks Applications in aeolian environments Applications in loessic environments Applications in glacial and periglacial environments Applications in fluvial and hillslope environments Applications in coastal and marine environments Applications of luminescence dating to active tectonic contexts Applications in archaeological contexts Rock surface burial and exposure dating Future developments in luminescence dating Reviving Palmyra in Multiple Dimensions: Ahmet Denker, Gabriele Fangi, Minna Silver Caithness Archaeology J. Heald Soil and Rock Description in Engineering Practice David Norbury Logging the Chalk Rory N.

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