Bookbot

Geophysical Monograph - 95: Earth Processes

Reading the Isotopic Code

Guardar

Parámetros

  • 437 páginas
  • 16 horas de lectura

Más información sobre el libro

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).

Compra de libros

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

Idioma
Publicado en
1996
Encuadernación
(Tapa dura),
Estado del libro
Dañado
Precio
63,99 €

Métodos de pago

Nadie lo ha calificado todavía.Añadir reseña

Título
Geophysical Monograph - 95: Earth Processes
Subtítulo
Reading the Isotopic Code
Idioma
Inglés
Publicado en
1996
Formato
Tapa dura
Páginas
437
ISBN10
0875900771
ISBN13
9780875900773
Serie
Etiquetas
Ciencia, Geología
Descripción
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).