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During the 19th century, and even well into the twentieth, geological chronology was very crude.Dates were estimated according to the supposed rate of deposition of rocks, and figures of several hundred million years were bandied out; usually arrived at through inspired guesswork rather than anything else.So a 40,000 year C-14 date and a 60,000 year thermoluminescence date could easily come from the same strata, right next to each other, and possibly reflect a date of anything between 30,000 and 70,000 calendar years depending on the standard deviations of your dates.Some thermoluminescence dates that are in the order of 50,000 years /- 25,000 years, which with a two standard deviation limit puts it anywhere between yesterday and 100,000 years ago.The radioactive isotope Carbon 14 has a half-life of 5,730 years.This has made it useful for measuring prehistory and events occurring within the past 35 to 50 thousand years.
If the sample is 75% U-235 and 15% Lead (and 10% other), then the sample is approximately 300 mya.For example, Uranium (U-235 or U-238) runs into the Thorium series then breakdowns into Radium and Radon, and finally, into Lead (the stable isotope).Volcanic tuft containing U-235 also contains (stable) Lead associated directly with it.Here are the half-lives of some other radioactive elements: These are said to be used in dating techniques of gas formation light emission called thermoluminescence).Besides thermoluminescence there is also the measurement of the ratio of the radioactive material to its decay elements.



Any further back than that and your standard deviations go way up.
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