Bookbot

Geophysical Monograph - 95: Earth Processes

Reading the Isotopic Code

Enregistrer

Paramètres

  • 437pages
  • 16 heures de lecture

En savoir plus sur le livre

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 close-2.9 Ga (Gerling, 1942), closer-3.0 Ga (Holmes, 1949) and closest-4.50 Ga (Patterson, Tilton and Inghram, 1953).

Achat du livre

Geophysical Monograph - 95: Earth Processes, Asish Basu, Stan Hart

Langue
Année de publication
1996
Reliure
(rigide),
État du livre
Abîmé
Prix
63,99 €

Modes de paiement

Personne n'a encore évalué .Évaluer

Titre
Geophysical Monograph - 95: Earth Processes
Sous-titre
Reading the Isotopic Code
Langue
Anglais
Publié
1996
Format
rigide
Pages
437
ISBN10
0875900771
ISBN13
9780875900773
Séries
Mots clés
Science, Géologie
Description
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 close-2.9 Ga (Gerling, 1942), closer-3.0 Ga (Holmes, 1949) and closest-4.50 Ga (Patterson, Tilton and Inghram, 1953).