Radiometric dating blind test

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The rate of helium leakage depends primarily on temperature.The higher the temperature, the greater the leakage. Helium leakage can be measured in core samples from various depths down as far as a few miles below the surface.In addition to measuring U-Pb decay to date rock, other techniques include measuring K.Geologists do not normally use multiple measurement methods on the same sample.[RATE Conference: predicted in 2000, measured in 2001] The obvious discrepancy between U-PB dating and helium leakage dating in the same samples requires us to look for some way to reconcile. Pressure was factored into measurements of mica and biotite from the core samples.The possibly flawed assumptions with U-PB decay have already been described, so the potential flaws with helium leakage must be considered. To fit the billion year model, the temperature at 3 miles below the surface would have to have been somewhere below –40C at the time of formation. Helium does not diffuse from surrounding biotite into zircons and the average helium content in surrounding biotite is 1/200 that of helium in zircons. The only other known viable argument is that leakage is increased by additional crystal damage due to radioactive decay.The precise methods of decay vary, but the principle for determining age is generally the same.

This means the halos must have formed at about the same time.Various rock samples have plentiful fission tracks useful for measuring rock age.Although ages vary from a few million to several hundred million years, the first and most obvious conclusion is that abundant nuclear decay occurred during the formation of the rock strata.The initial nuclide (proton and neutron) quantities and relative ratios must be assumed.These assumptions, particularly the notion you can know with any degree of certainly the original nuclide ration, are very bold indeed regardless of your beliefs about the past. Uranium and its various daughter products are frequently found as impurities in crystal zirconium (Zr Si O.

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