Evolution of early crust in chondritic or non-chondritic Earth inferred from U-Pb and Lu-Hf data for chemically abraded zircon from the Itsaq Gneiss Complex, West Greenland

Zircon grains in rocks collected from the Itsaq Gneiss Complex, southwest Greenland, were analyzed for U-Pb and Lu-Hf in the same grain using isotope dilution - thermal ionization mass spectrometry (TIMS) and multicollector - inductively coupled plasma -

Bibliographic Details
Main Authors: Amelin, Yuri, Kamo, Sandra L, Lee, Der-Chuen
Format: Article in Journal/Newspaper
Language:unknown
Published: N R C Research Press 2015
Subjects:
Online Access:http://hdl.handle.net/1885/67513
Description
Summary:Zircon grains in rocks collected from the Itsaq Gneiss Complex, southwest Greenland, were analyzed for U-Pb and Lu-Hf in the same grain using isotope dilution - thermal ionization mass spectrometry (TIMS) and multicollector - inductively coupled plasma -