The rubidium strontium dating. There was a problem with your submission.

The rubidium-strontium dating method is a radiometric dating technique used by scientists to determine the age of rocks and minerals from the quantities they contain of specific isotopes of rubidium (87Rb) and strontium (87Sr, 86Sr).

Therefore the amount of argon formed provides a direct measurement of the amount of potassium present in the specimen when it was originally formed. Part of Springer Nature. Where the isochron crosses the vertical axis corresponds to a hypothetical sample with no rubidium at all. Apparently, he did know better, because he qualifies the exposition in a footnote stating:. In other examples, the ages of rocks with insufficient rubidium for dating have been successfully determined. Index Reference Jelley Sec 3.

In some cases, partly reset systems also may be detected.

The slope of the isochron line gives a measurement of the time since the last complete melting of the rock. Weathering is a disturbing influence, as is leaching or exchange by hot crustal fluids, since many secondary minerals contain rubidium. The resulting Rb-Sr ratios and Rb and Sr abundances of both the whole rocks and their component minerals will be markedly different.

This is well known for the Cenozoic time-scale but, due to poorer preservation of carbonate sequences in the Mesozoic and earlier, it is not completely understood for older sequences. Strontium occurs naturally as a mixture of several nuclides, including the stable isotope strontium Where the isochron crosses the vertical axis corresponds to a hypothetical sample with no rubidium at all.

Answers to YEC Arguments - Episode 44 - Rubidium-Strontium Dating

F, the fraction of K40 remaining, is equal to the amount of potassium in the sample, divided by the sum of potassium in the sample plus the calculated amount of potassium required to produce the amount of argon found. In old rocks, there will be less potassium present than was required to form the mineral, because some of it has been transmuted to argon. The rubidiumâ€”strontium pair is ideally suited for the isochron dating of igneous rocks. Importance of Rb-Sr dating6. There is considerable promise for dating garnet , a common metamorphic mineral, because it is known to concentrate the parent isotope.

In fact, if just an average of the point-to-point slopes for all the data points is used, including the Homestead meteorite, an age of 4.