# Dating age range equation derivation, how Old is the Earth

Second, mixing is a mechanical process that is physically possible only in those rock systems where two or more components with different chemical and isotopic compositions are available for mixing. Are wormholes, subspace, hyperspace, slipstreams, corridors or conduits, warp speeds, trans-warp, folding of space, bridges, portals and gateways, or inter-dimensional travel real? This results in an identical Y-value for the data points representing each mineral matching the Y-value of the source material. One twin has to change frames, leading to different proper times in the twin's world lines. But the computed age is not affected.

Isochron methods avoid the problems which can potentially result from both of the above assumptions. The only reasonably common way is by mixing of materials. No parent isotope or daughter isotope has entered or left the sample since its time of formation.

This is an important point. We can only speculate on where Kofahl and Segraves obtained their numbers. Standard values are used, based on direct measurements. In fact, negative slopes are exceedingly rare and are confined to those types of systems, mentioned above, in which mechanical mixing is possible and evident.

Mineral composition and the sequence of mineral formation are governed by chemical laws and do not involve mixing. An exception is the lava from the Hualalai flow, which is so badly contaminated by the xenoliths that it is impossible to obtain a completely inclusion-free sample. This will be discussed in more detail in the section on Gill's paper below. Research on quantum entanglement as it relates to gravity.

Gamma rays very small bundles of energy are the device by which an atom rids itself of excess energy. In the field, they look like large raisins in a pudding and even occur in beds piled one on top of the other, glued together by the lava.

It is clear that there is no increase in the values as a function of time. Rb and Sr are quite different elements and are incorporated into the various minerals in varying proportions according to the composition and structure of the minerals. Have you considered below unexplained supernatural events? In addition, it requires that these measurements be taken from several different objects which all formed at the same time from a common pool of materials. The slope of the line is the ratio of enriched D to remaining P.

Both are trace elements and rarely form minerals of their own. However, the interval between two events can also correspond to the proper time of accelerated clocks present at both events. As discussed above in the section on Rb-Sr dating the simplest form of Rb-Sr dating i.

As a result, the data points with the most P the right-most ones on the plot move the greatest distance per unit time. Second, Slusher has confused isotopes and elements. Movement of data points as decay occurs. Certainly this is not produced by an influx from outer space. The amount of P in each sample, and The extent to which it is enriched in D, relative to Di.

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References Generic Radiometric Dating The simplest form of isotopic age computation involves substituting three measurements into an equation of four variables, and solving for the fourth. Initial daughter product The amount of initial D is not required or assumed to be zero. Measurements of decay rates under differing gravitational and magnetic fields also have yielded negative results. This is computed from the current quantity of parent isotope plus the accumulated quantity of daughter isotope.

It depends on the accuracy of the measurements and the fit of the data to the line in each individual case. Differential migration of elements as minerals form.

Those who struggle with parallax reality might read about it in the linked wikipedia article. In contrast, P is a different element with different chemical properties. Can angels or aliens travel up to or faster than light speed?

Pnow - The quantity of the parent isotope that remains now. So, are isochron methods foolproof? There is a fourth type of decay that can be affected by physical and chemical conditions, though only very slightly. Consider an old body of rock as evidenced by its good fit to an isochron with distinctly non-zero slope with minerals which melt at different temperatures. In other words, random gain or loss of P does not affect a zero-age isochron.

Next we shall examine in detail some specific examples. The individual lava flows are not cogenetic. Beta decay involves the ejection of a beta particle an electron from the nucleus.

Loss of P destroys the fit to a line. If the results were essentially random numbers, that would not be the expected distribution of results. Two cases where it appears that the half life is increasing with time are as follows.

## How Old is the Earth

Such samples are rare, and so nearly all modern Rb-Sr dating is done by the isochron method. The large majority of isochron dating results are in accordance with the mainstream age and history of the Earth. The resulting age is meaningful, but it does not have the meaning which one might expect for the dating result i. Studies such as the one by Funkhouser and Naughton are routinely done to ascertain which materials are suitable for dating and which are not, puchar katalonii online dating and to determine the cause of sometimes strange results. Does this leave room to discard isochron dating as entirely unreliable?

It might instead be the original time at which the samples became separated from a common pool of matter, or the age of that source material itself. Because these types of radioactive decay occur spontaneously in the nucleus of an atom, the decay rates are essentially unaffected by physical or chemical conditions. In nearly every case, the measured K-Ar age was zero, as expected if excess argon is uncommon.

Such assumptions will not always be accurate in the real world. The Rb-Sr isochron method is most commonly used on igneous rocks, which form by cooling from a liquid. In the real world, nothing is perfect. Data points of individual mineral samples show scatter due to chemical differentiation at the last time of melting.

The range of uncertainty varies, and may be as much as an order of magnitude different from the approximate value above. This results in a range of X-values for the data points representing individual minerals. In most cases, any age less than about P half-lives will include zero within its range of uncertainty. The xenoliths, which vary in composition and range in size from single mineral grains to rocks as big as basketballs, do, indeed, carry excess argon in large amounts. That quantity of D could be subtracted out of each sample, and it would then be possible to derive a simple age by the equation introduced in the first section of this document for each sample.

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