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  2. Uranium–lead dating - Wikipedia

    en.wikipedia.org/wiki/Uraniumlead_dating

    Uraniumlead 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.

  3. Radiometric dating - Wikipedia

    en.wikipedia.org/wiki/Radiometric_dating

    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 ...

  4. Detrital zircon geochronology - Wikipedia

    en.wikipedia.org/wiki/Detrital_zircon_geochronology

    Detrital zircon geochronology has become increasingly popular in geological studies from the 2000s mainly due to the advancement in radiometric dating techniques. [ 1 ] [ 2 ] Detrital zircon age data can be used to constrain the maximum depositional age, determine provenance , [ 3 ] and reconstruct the tectonic setting on a regional scale.

  5. Geochronology - Wikipedia

    en.wikipedia.org/wiki/Geochronology

    Monazite geochronology is another example of U–Pb dating, employed for dating metamorphism in particular. Uraniumlead dating is applied to samples older than about 1 million years. Uranium–thorium dating. This technique is used to date speleothems, corals, carbonates, and fossil bones. Its range is from a few years to about 700,000 years.

  6. Lead–lead dating - Wikipedia

    en.wikipedia.org/wiki/Leadlead_dating

    Leadlead 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samples, normally based on 'whole-rock' samples of material such as granite.For most dating requirements it has been superseded by uraniumlead dating (U–Pb dating), but in certain specialized situations (such as dating meteorites and the age of the Earth) it is more important than U–Pb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.

  7. Thermochronology - Wikipedia

    en.wikipedia.org/wiki/Thermochronology

    Fission track dating is the method used in thermochronology to find the approximate age of several uranium-rich minerals, such as apatite. When nuclear fission of uranium-238 ( 238 U ) happens in inorganic materials, damage tracks are created.

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  9. Category:Radiometric dating - Wikipedia

    en.wikipedia.org/wiki/Category:Radiometric_dating

    Download as PDF; Printable version; In other projects ... Pages in category "Radiometric dating" The following 30 pages are in this category, out of 30 total ...