Potassium—argon decay constants and age tables

Author:

Smith Alan Gilbert1

Affiliation:

1. Department of Geology, Sedgwick Museum Cambridge

Abstract

SummaryThis paper outlines the physical measurements that determine the potassium–argon decay constants; compares the constants currently in use with those derived from the best physical measurements; and shows the magnitude of error in the time-scale due to different estimates of the constants and to a 5 per cent error in each of the constants. Tables are given which can be used by the non-specialist to relate K–Ar ages directly to the experimentally determined argon/potassium ratios using ‘standard’ constants.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference17 articles.

1. PRECAMBRIAN AGES IN THE WIND RIVER MOUNTAINS, WYOMING

2. Recent work on the radioactivity of potassium and some related geophysical problems;Birch;J. geophys. Res.,1951

3. Energy Levels of Light Nuclei (Z=11toZ=20)

4. On the choice of decay contents of K40 for the determination of the ages of rocks by the ratio of Ar40 to K40;Firsov;Bull. Acad. Sci. U.R.S.S. (Ser. Geol. & Geophys.),1960

5. Potassium–argon time scale;Folinsbee;Int. geol. Congr.,1960

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