Optically Stimulated Luminescence Dating

Optically Stimulated Luminescence Dating




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In physics, optically stimulated luminescence (OSL) is a method for measuring doses from ionizing radiation . It is used in at least two applications: Luminescence dating of ancient materials: mainly geological sediments and sometimes fired pottery, bricks etc ., although in the latter case thermoluminescence dating is used more often
www .usu .eduΒ β€ΊΒ geo β€Ί luminlab β€Ί whatis .html
OSL is an acronym for Optically-Stimulated Luminescence . Optically-Stimulated Luminescence is a late Quaternary dating technique used to date the last time quartz sediment was exposed to light . As sediment is transported by wind, water, or ice, it is exposed to sunlight and zeroed of any previous luminescence signal .
Optically stimulated luminescence (OSL) is a technique used to date fossils in geological sediments through ionized radiation to determine the last time a mineral was exposed to sunlight . OSL assumes that minerals were both constantly and sufficiently exposed to oxygen before being buried, noticeably bleaching the observed mineral or fossil .
Optical dating differs from thermoluminescence (TL) dating in that visible/infrared light from lasers or LEDs (light-emitting-diodes) is used as a means of stimulation, in contrast to thermal stimulation . It has several advantages over TL dating : (i) the resetting of the OSL ( optically stimulated luminescence ) clock is more effective than that of TL
www .antarcticglaciers .orgΒ β€ΊΒ glacial-geology β€Ί dating-glacial-sediments-2 β€Ί optically-stimulated-luminescence
Another way of dating glacial landforms is optically stimulated luminescence dating (OSL) . OSL is used on glacial landforms that contain sand, such as sandur or sediments in glacial streams . The OSL signal is reset by exposure to sunlight, so the signal is reset to zero while the sand is being transported (such as in a glacial meltwater stream) .
This paper aims to provide an overview concerning the optically stimulated luminescence (OSL) dating method and its applications for geomorphological research in France . An outline of the general physical principles of luminescence dating is given .
Optically stimulated luminescence (OSL) dating is one of several techniques that make use of the ability of some natural crystalline materials to store energy, in the form of trapped charge, over long periods . The most widely used of these materials are the insulators quartz and feldspar .
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 , infrared stimulated luminescence , and thermoluminescence dating . "Optical dating " typically refers to OSL and IRSL, but not TL .
Luminescence dating (including thermoluminescence and optically stimulated luminescence ) is a type of dating methodology that measures the amount of light emitted from energy stored in certain rock types and derived soils to obtain an absolute date for a specific event that occurred in the past .
[1] Optically stimulated luminescence (OSL) dating is now widely accepted as a chronometer for terrestrial sediment . More recently, it has been suggested that OSL may also be useful in the dating of deep-sea marine sediments .
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Optically Stimulated Luminescence Dating












































































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