Early Archean crustal evolution of the Jack Hills Zircon source terrane inferred from Lu–Hf, 207Pb/206Pb, and δ18O systematics of Jack Hills zircons-Reference-Cited by-同舟云学术

Early Archean crustal evolution of the Jack Hills Zircon source terrane inferred from Lu–Hf, 207Pb/206Pb, and δ18O systematics of Jack Hills zircons

Published:2011-09 Issue:17 Volume:75 Page:4816-4829
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Bell Elizabeth A.,Harrison T. Mark,McCulloch Malcolm T.,Young Edward D.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference52 articles.

1. Geochronology of the Jack Hills detrital zircons by precise U–Pb isotope dilution analysis of crystal fragments;Amelin;Chem. Geol.,1998

2. Meteorite phosphates show constant Lu-176 decay rate since 4557 million years ago;Amelin;Science,2005

3. Early-Middle Archean crustal evolution deduced from Lu–Hf and U–Pb isotopic studies of single zircon grains;Amelin;Geochim. Cosmochim. Acta,2000

4. Nature of the Earth’s earliest crust from hafnium isotopes in single detrital zircons;Amelin;Nature,1999

5. Combined Sm–Nd isotopic systematics and U–Pb zircon characteristics in the Narryer Gneiss complex, Western Australia: implications for Archean crustal genesis;Bennett;Intl. Archean Symp.,1990

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