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So with their encouragement I will attempt to explain the method and the criteria used to interpret the data generated from a Ar step-heating experiment.
The results from this sample are an excellent example of the advantages of Ar methods of dating have been successfully applied to many fundamental Earth science problems, including the establishment and calibration of the Geomagnetic Polarity Time Scale (GPTS), calibration of the Paleontological Time Scale (PTS), calibration of Hominid evolution, and numerous tectonic studies.
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In addition, faunal succession and the use of "key" diagnostic fossils were used to correlate lithologic units over wide geographic areas.
Although lithologic units could be placed within a known sequence of geologic periods of roughly similar age, absolute ages, expressed in units of years, could not be assigned.
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For a complete discussion on the development of the Geologic time scale see Berry, (1968).