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#Post#: 93--------------------------------------------------
GB/K-Ar DATING
By: Admin Date: February 2, 2017, 6:37 pm
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Guy Berthault
Addendum
HTML http://sedimentology.fr
....................... Ar (ppm)
dacite 350,000 years
feldspar 340,000 years
amphibole 900,000 years
pyroxene 1,700,000 to 2,800,000 years
according to the model age equation.
The report says “these ages, of course, are preposterous. The
fundamental dating assumption (no radiogenic argon was present
when the rock formed) is questioned by these data. Instead data
from the Mt. St. Helens dacite, argue that significant “excess
argon” was present when the lava solidified in 1986. Phenocrysts
of orthopyroxene, hornblende and plagioclase, are interpreted
to have occluded argon within their mineral structure deep in
the magma chamber and to have retained the argon after
emplacement and solidification of the dacite. Orthopyroxene
retains the most argon, followed by hornblende, and finally
plagioclase”.
The presence of abundant argon deep in the rocks produced at the
time of the eruption (recent or ancient) and which rises
towards the surface of the magma, gives the impression the
rocks are older than they are when dated by the potassium/argon
method.
The fact that the method has been used to date the
Australopithecines raises the question: what then is their real
age?
This fundamental dating assumption, as regards other radiometric
dating is also questioned, because every sample rock contains a
quantity of daughter resulting from the decay of the parent in
the lava, before crystallisation, which makes the rock appear
older. The model age equation requires that the initial number
of daughter atoms be known. No analytical equipment, however,
can give this value.
The isochron age equation depends on several assumptions, the
principal being that rocks of a same formation, when they
formed, had the same abundance of daughter, in this case argon.
This is not so for the dacite and its components mentioned above
which only ten years after the eruption showed different
respective quantities of argon.
The model age so determined corresponds to magma and not
crystallisation (as for the dacite). Moreover, gravitational
settling between minerals exists in the cooling magma. For
example, strontium, which has the same valence and very similar
ionic radius substitutes for calcium. So in fact, since
plagioclase which carries strontium is less dense than olivine,
then due to gravitational settling in an intrusion the greatest
quantity of plagioclase and therefore strontium can sometimes
remain in the higher levels of that intrusion. So strontium can
be more abundant at a higher level in a magma intrusion which
gives an apparently older age.
In conclusion the radioactive age does not necessarily refer to
the crystallisation of rocks and consequently not to geological
dating.
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