Potassium argon dating granite

Reheating events and diffusion of argon from the boundaries of the grain can result in lower Ar date.Sometimes, when a large amount of argon has been lost, this is not possible.A very short time for emplacement of the Yellowknife granite series, ranging from hornblende-biotite diorite to muscovite granite, is inferred.Results given for two unseparated granites and a feldspar phenocryst from the Sierra Nevada batholith confirm earlier lead-alpha activity determinations and an age near 100 m.y. Data on mica separates from this region are needed, however. for an upper middle Devonian (Givetian) potash salt from western Canada is thought to be a useful addition to age data on rocks from the palaeontologically controlled portion of the geological time scale and is in agreement with the time scale of HOLMES.Both the physical geologists and paleontologists could point to evidence that much more time was needed to produce what they saw in the stratigraphic and fossil records.As one answer to his critics, Kelvin produced a completely independent estimate -- this time for the age of the Sun.First results in an extensive programme in potassium-argon dating at Berkeley arc reported.Ultra-high-vacuum techniques have been incorporated in the argon extraction apparatus and in a new mass spectrometer especially designed for these researches.

However, scientists discovered that it was possible to turn a known proportion of the potassium into argon by irradiating the sample, thereby allowing scientists to measure both the parent and the daughter in the gas phase.

There are several steps that one must take to obtain an argon-argon date: First, the desired mineral phase(s) must be separated from the others.

Common phases to be used for argon-argon dating are white micas, biotite, varieties of potassium feldspar (especially sanidine because it is potassium-rich), and varieties of amphibole. This can be used to solve equation 2 for the sample.

The coincidence of the ages of the different fractions of the granite and xenolith samples is discussed in the light of the different suggestions about the age of the Malmesbury sediments.

The conclusion is reached that all pre-granitization history has been eliminated.

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