Optically Stimulated Luminescence Dating Definition
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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 .
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
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 .
www .antarcticglaciers .orgΒ βΊΒ glacial-geology βΊ dating-glacial-sediments-2 βΊ optically-stimulated-luminescence
Optically Stimulated Luminescence (OSL) is a technique used for dating sand grains, often used in glacial outwash landforms .
Optical: Relating to the use of visible or near-visible light . Stimulated : To excite with a stimulus (light or heat) Luminescence : The emission of light . Optically stimulated luminescence : The emission of light from crystalline materials when stimulated by light following previous absorption of energy from radiation .
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 .
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 .
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 .
What is Luminescence Dating ? Luminescence dating is a form of geochronology that measures the energy of photons being released . In natural settings, ionizing radiation (U, Th, Rb, & K ) is absorbed and stored by sediments in the crystal lattice . This stored radiation dose can be evicted with stimulation and released as luminescence .
Luminescence dating is a geochronological technique used to directly date geological events and archeological artifacts from the late Quaternary period (Walker, 2005) . The technique was first developed in the 1960s, with the aim of dating archeological ceramics to determine the time elapsed since firing (using thermoluminescence, TL, dating ) .
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Optically Stimulated Luminescence Dating Definition
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