Optically-Stimulated Luminescence is a late Quaternary dating technique used to date the last time quartz sediment was exposed to light. Luminescence dating refers to a group of methods of determining how long ago mineral grains were last exposed to sunlight or sufficient heating. It is useful to geologists and archaeologists who want to know when such an event occurred. It uses various methods to stimulate and measure luminescence. It includes techniques such as optically stimulated luminescence (OSL). Please reference: Mallinson, D.
This paper aims to provide an overview concerning the optically stimulated luminescence OSL dating method and its applications for geomorphological research in France. This paper aims to provide an overview concerning the optically stimulated luminescence (OSL) dating method and its applications for geomorphological. Over the last 60 years, luminescence dating has developed into a robust chronometer for applications in earth sciences and archaeology.
Luminescence dating refers to a group of methods of determining how long ago mineral grains were last exposed to sunlight or sufficient heating. OSL has been widely used to date glacial be used effectively with other dating techniques. Introduction How do we measure the OSL signal?
Optical dating of sediment using optically stimulated luminescence has technique complements other Quaternary dating methods, including.
Luminescence dating is a scientific method which dates certain artifacts by measuring the amount of light energy they have trapped.
A Brief Description of Optically Stimulated Luminescence Dating, acnenomorereviewed.info edu/geology/mallinsond/OSL, if use of Figure 1 is desired. Optically stimulated.
resetting of the OSL (optically stimulated luminescence) clock is more effective than The luminescence dating techniques estimate the time of the most recent .