STUDIES ON THE LEAD METHOD OF AGE DETERMINATION, PART 1
Ages of a number of radioactive minerals have been determined from Pb207/Pb206, Pb206/U238, Pb207/U235 and Pb206/Pb210 ratios. Values obtained for minerals from classic localities agree well with those reported by other investigators. Major attention has been given to the anomalies of the ages of a given mineral computed from the various possible isotope ratios. The development of the Pb210 method adds greatly to the fund of data required to obtain accurate ages. The 206/210 age is essentially independent of uranium leaching or radoff leakage. The latter is a significant factor in 206/238 and 207/206 ratios and must be measured experimentally to evaluate ages from these ratios. It appears that throughout most of the span of geologic time the 207/235 and 206/210 ages are the most reliable. The 206/238 supersedes the 207/235 age in accuracy for very young minerals. The 207/206 age does not merit the reliability ascribed to it by earlier investigators.
- Research Organization:
- Lamont Geological Observatory, Columbia Univ.
- NSA Number:
- NSA-08-001351
- OSTI ID:
- 4421453
- Report Number(s):
- NYO-6199
- Country of Publication:
- United States
- Language:
- English
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