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Abstracts of the Eighth International Conference on Geochronology, Cosmochronology, and Isotope Geology
  • Language: en
  • Pages: 384
Seventh International Conference on Geochronology, Cosmochronology and Isotope Geology
  • Language: en
  • Pages: 125
Short Papers of the Fourth International Conference, Geochronology, Cosmochronology, Isotope Geology
  • Language: en
  • Pages: 476
Fifth International Conference on Geochronology, Cosmochronology, Isotope Geology
  • Language: en
  • Pages: 427

Fifth International Conference on Geochronology, Cosmochronology, Isotope Geology

  • Type: Book
  • -
  • Published: 1983
  • -
  • Publisher: Unknown

None

Abstracts of the Eighth International Conference on Geochronology, Cosmochronology, and Isotope Geology
  • Language: en
  • Pages: 398

Abstracts of the Eighth International Conference on Geochronology, Cosmochronology, and Isotope Geology

Abstracts taken from 1994 conference in Geochronology, Cosmochronology and Isotope Geology. Abstracts are organized alphabetically by first author and were printed as recieved from the author-prepared copy. The Author index is comprehensive and includes all authors.

Terrestrial Noble Gases
  • Language: en

Terrestrial Noble Gases

  • Type: Book
  • -
  • Published: 1985
  • -
  • Publisher: Unknown

None

Earth Processes
  • Language: en
  • Pages: 444

Earth Processes

Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 95. Publication of this monograph will coincide, to a precision of a few per mil, with the centenary of Henri Becquerel's discovery of "radiations actives" (C. R. Acad. Sci., Feb. 24, 1896). In 1896 the Earth was only 40 million years old according to Lord Kelvin. Eleven years later, Boltwood had pushed the Earth's age past 2000 million years, based on the first U/Pb chemical dating results. In exciting progression came discovery of isotopes by J. J. Thomson in 1912, invention of the mass spectrometer by Dempster (1918) and Aston (1919), the first measurement of the isotopic composition of Pb (Aston, 1927) and the final approach, using Pb-Pb isotopic dating, to the correct age of the Earth: close-2.9 Ga (Gerling, 1942), closer-3.0 Ga (Holmes, 1949) and closest-4.50 Ga (Patterson, Tilton and Inghram, 1953).