Artículo:

Magmatic and Crustal Differentiation History of Granitic Rocks from Hf-O Isotopes in Zircon

Autor:

A. I. S. Kemp

C. J. Hawkesworth

G. L. Foster

Resumen:

Hafnium and oxygen isotopes in zircon crystals imply that common granites form by recycling crustal material in mantle-derived magmas, not by remelting deep crustal rocks

Página:

980

Sección:

Reports

Publicación:

Science

Volúmen:

315

Número:

5814

Fecha:

16 February 2007

ISSN:

00368075

SrcID:

00368075-2007-02-16.txt