Optically stimulated luminescence dating wiki
Chronostratigraphy is similar to biostratigraphy, but it attempts to assign an absolute age for a particular fossil assemblage.
Geochronological units are referred to as periods of time when chronostratigraphic units are only referred to in their geological context Ages of minerals can be determined by measuring the number of radiogenic daughter isotopes compared to the parent isotopes.
"Optical dating" typically refers to OSL and IRSL, but not TL.This recharge can be measured and compared to the latent luminescent signal.Luminescence dating refers to a group of methods of determining how long ago mineral grains were last exposed to sunlight or sufficient heating.There are many different dating methods that can be used to determine the age of rocks, fossils, and sediments, and the advancement of modern technology is allowing faster determination of more accurate age measurements.The ages can be determined either absolutely using radioactive isotopes or relatively using dating methods such as index fossils, global stable isotopic trends, and paleomagnetism.
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