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U—Th—Pb Dating of Minerals

  • D. Gebauer
  • M. Grünenfelder

Abstract

Natural U consists of two radioactive parent-isotopes, 238U and 235U, the half-lives of which fall into the range of geologic time. Outside this range is the half-life of 232Th, which represents the only natural isotope of Th.

Keywords

Detrital Zircon Concordia Diagram Zircon Population Metamorphic Overprint French Central Massif 
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© Springer-Verlag Berlin Heidelberg 1979

Authors and Affiliations

  • D. Gebauer
  • M. Grünenfelder

There are no affiliations available

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