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Uranium–lead dating, abbreviated U–Pb dating, is one of the oldest [1] and most refined of the radiometric dating schemes. It can be used to date rocks that formed and crystallised from about 1 million years to over 4.5 billion years ago with routine precisions in the 0.1–1 percent range. [2] [3] The method is usually applied to zircon.
One of its great advantages is that any sample provides two clocks, one based on uranium-235's decay to lead-207 with a half-life of about 700 million years, and one based on uranium-238's decay to lead-206 with a half-life of about 4.5 billion years, providing a built-in crosscheck that allows accurate determination of the age of the sample ...
Zircon is extremely useful for geological dating: when forming, it collects tiny imperfections of uranium, but never lead. It follows that if lead is present in zircon, it must have come from decay of the uranium present. (The process is known as U-Pb dating.) The team measured the concentrations and isotopic compositions of foreign elements ...
Pages in category "Radiometric dating" The following 30 pages are in this category, out of 30 total. ... Uranium–lead dating; Uranium–thorium dating;
Lead–lead dating is a method for dating geological samples, normally based on 'whole-rock' samples of material such as granite.For most dating requirements it has been superseded by uranium–lead dating (U–Pb dating), but in certain specialized situations (such as dating meteorites and the age of the Earth) it is more important than U–Pb dating.
Zircon is a strong tool for uranium-lead age determination because of its inherent properties: [8] Zircon contains high amount of uranium for machine recognition, commonly 100–1000 ppm. [8] Zircon has a low amount of lead during crystallization, in parts per trillion. [8] Thus, lead found in zircon can be assumed as daughter nuclei from ...
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The following year, Boltwood made the assertion that lead was the final decay product in the disintegration of uranium, and that Pb:U ratios increase in older geological samples. In 1907, he published results of analyzing ten mineral samples from different world locations, including a thorianite [ 2 ] that measured 2.2 billion years old.