放射性定年法 Radiometric dating


![Sm/Nd isochron plotted of samples [13] from the Great Dyke, Zimbabwe. The age is calculated from the slope of the isochron (line) and the original composition from the intercept of the isochron with the y-axis.](/uploads/202501/21/Sm_Nd_Great_Dyke_Isochron4057.png)
![A concordia diagram as used in uranium-lead dating, with data from the Pfunze Belt, Zimbabwe.[17] All the samples show loss of lead isotopes, but the intercept of the errorchron (straight line through the sample points) and the concordia (curve) shows the correct age of the rock.[12]](/uploads/202501/21/Pfunze_belt_concordia4057.png)
放射测年法是利用测定被测定物中某些放射性元素与其衰变产物的比率,之后应用这种放射性元素半衰期计算年代的方法。
单词 | Isotopic dating |
释义 |
Isotopic dating
中文百科
放射性定年法 Radiometric dating(重定向自Isotopic dating)
![]() ![]() ![]() ![]() 放射测年法是利用测定被测定物中某些放射性元素与其衰变产物的比率,之后应用这种放射性元素半衰期计算年代的方法。
英语百科
Radiometric dating 放射性定年法(重定向自Isotopic dating)
![]() ![]() ![]() ![]() Radiometric dating or radioactive dating is a technique used to date materials such as rocks or carbon, in which trace radioactive impurities were selectively incorporated when they formed. The method compares the abundance of a naturally occurring radioactive isotope within the material to the abundance of its decay products, which form at a known constant rate of decay. The use of radiometric dating was first published in 1907 by Bertram Boltwood and is now the principal source of information about the absolute age of rocks and other geological features, including the age of the Earth itself, and can be used to date a wide range of natural and man-made materials. |
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