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| | [No title] (Site not responding. Last check: 2007-10-11) |
 | | In other minerals present in the same rock, which may have different initial amounts of primordial strontium, the proportion of strontium to rubidium will differ (since they have different amounts of rubidium), but the ratio of the strontium isotopes to each other will be the same, since they are chemically identical and cannot be separated. |
 | | In this method, there is no need to estimate the amount of daughter element that may have contaminated the sample, because if any strontium or rubidium has been removed or added from the original rock, this will produce a point that lies outside the isochron line, thus indicating that the sample has been contaminated. |
 | | In any case, both the potassium-argon and the rubidium- strontium methods present precise methods of determining the amount of radiogenic daughter element, and the isochron method provides a precise method of checking for contamination. |
| www.geocities.com /CapeCanaveral/Hangar/2437/radiodte.htm (3000 words) |
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