Uranium—lead datingabbreviated U—Pb datingis one of the oldest  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. The dating method is usually performed on the mineral zircon. The mineral incorporates uranium and thorium atoms into its crystal structurebut strongly rejects lead. Lead isotope dating geology, one can assume that the entire lead content of the zircon is radiogenici. Thus the current ratio of lead to uranium in the mineral can be used to determine its age.
The method relies on two separate decay chainsthe uranium series from U to Pb, with a half-life of 4.
The above uranium to lead decay routes occur via a series of alpha and beta decays, in which U with daughter nuclides undergo total eight alpha and six beta decays whereas U with daughters only experience seven alpha and four beta decays.
Lead isotope dating geology of two 'parallel' uranium—lead decay routes U to Pb and U to Pb leads to multiple dating techniques within the overall U—Pb system.
The term U—Pb dating normally implies the coupled use of both decay schemes in the 'concordia diagram' see below.
However, use of a single decay scheme usually U to Pb leads to the U—Pb isochron dating method, analogous to the rubidium—strontium dating method. Finally, ages can also be determined from the U—Pb system by analysis of Pb isotope ratios alone. This is termed the lead—lead dating method.
Clair Cameron Pattersonan American geochemist who pioneered studies of uranium—lead radiometric dating methods, is famous for having used it to obtain one of the earliest estimates of the age of the Earth. Although zircon ZrSiO 4 is most commonly used, other minerals such as monazite see: Where crystals such as zircon with uranium and thorium inclusions do not occur, a better, more inclusive, model of the data must be applied.
These types of minerals often produce lower precision ages than igneous and metamorphic minerals traditionally used for age dating, but are more common in the geologic record. During the alpha decay steps, the zircon crystal "Lead isotope dating geology" radiation damage, associated with each alpha decay.
This damage is most concentrated around the parent isotope U and Thexpelling the daughter isotope Pb from its original position in the zircon lattice. In areas with a high concentration of the parent isotope, damage to the crystal lattice is quite extensive, "Lead isotope dating geology" will often interconnect to form a network of radiation damaged areas.
These fission tracks inevitably act as conduits deep within the crystal, thereby providing a method of transport to facilitate Lead isotope dating geology leaching of lead isotopes from the zircon crystal. Under conditions where no lead loss or gain from the outside environment has occurred, the age of the zircon can be calculated by assuming exponential decay of Uranium. These are said to yield concordant ages. Loss leakage of lead from the sample will result in a discrepancy in the ages determined by each decay scheme.
This effect is referred to as discordance and is demonstrated in Figure 1. If a series of zircon samples has lost different amounts of lead, the samples generate a discordant line.
The upper intercept of the concordia and the discordia line will reflect the original age of formation, while the lower intercept will reflect the age of the event that led to open system behavior and therefore the lead loss; although there has been some disagreement regarding the meaning of the lower intercept ages.
Zircon is very chemically inert and resistant to mechanical weathering—a mixed blessing for geochronologists, as zones or even whole crystals can survive melting of their parent rock with their original uranium-lead age intact. Zircon crystals with prolonged and complex histories can thus contain zones of dramatically different ages usually, with the oldest and youngest zones forming the core and rim, respectively, of the crystaland Lead isotope dating geology are said to demonstrate inherited characteristics.
Unraveling such complications which, depending on their maximum lead-retention temperature, can also exist within other minerals generally requires in situ micro-beam analysis via, say, ion microprobe SIMS or laser ICP-MS.
From Wikipedia, the free encyclopedia. The disintegration products of uranium: American Journal of Science Retrieved 7 January Alpha-recoil in U-Pb geochronology: Effective sample size matters.
Contributions to Mineralogy and Petrology4: Combined annealing and multi-step dissolution analysis for Improved precision and accuracy of zircon ages. Radiogenic Isotope Geology 2nd ed. Canon of Kings Lists of kings Limmu. Chinese Japanese Korean Vietnamese. Lunisolar Solar Lunar Astronomical year numbering. Deep time Geological history of Earth Geological time units.
Chronostratigraphy Geochronology Isotope geochemistry Law of superposition Luminescence dating Samarium—neodymium dating. Amino acid racemisation Archaeomagnetic dating Dendrochronology Ice core Incremental dating Lichenometry Paleomagnetism Radiometric dating Radiocarbon Uranium—lead Potassium—argon Tephrochronology Luminescence dating Thermoluminescence dating. Fluorine absorption Nitrogen dating Obsidian hydration Seriation Stratigraphy. Retrieved from Lead isotope dating geology https: Wikipedia articles needing clarification from October Views Read Edit View history.