Non isotopic dating
Georg-August-Universität Göttingen - Dendrochronology It has been used to calibrate C-14 dating, since C-14 production in the upper atmosphere depends on how much cosmic rays the Earth receives, which varies due to various factors.
So it is not a very "clean" test of radiometric dating.
In this regard, the Re–Os system to study the geochemical evolution of mantle rocks and in defining the chronology of mantle differentiation is extremely helpful.
Peridotite xenoliths which are thought to sample the upper mantle sometimes contain supra-chondritic Os-isotopic ratios.
Radiometric dating is also used to date archaeological materials, including ancient artifacts.
Different methods of radiometric dating vary in the timescale over which they are accurate and the materials to which they can be applied.
It is based on tree-ring counting and correlating the rings from different trees.
It has been possible to go back 10,000 years (8000 BCE) with this technique, which is 2000 years after the beginning of the Holocene Epoch.
We can see how do deal with this if we take a particular case. For example the amount of Rb in mantle rocks is generally low, i.e. The mantle thus has a low If these two independent dates are the same, we say they are concordant.Zircon grains are commonly partially or completely metamict, and therefore susceptible to Pb loss and common Pb contamination.Using Ca and K contents as indicators of damaged or contaminated zircon, a CHIME (Chemical U–Th–total Pb method) age of 347.8 ± 18 Ma was obtained from data with 0.0062 wt.% of Pb O.The Re-Os isochron plots the ratio of radiogenic Rhenium and Osmium were strongly refractory and siderophile during the initial accretion of the Earth which caused both elements to preferentially enter the Earth's core.Thus the two elements should be depleted in the silicate Earth yet the The reason for this apparent contradiction is owed to the change in behavior between Re and Os in partial melt events.