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 -
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
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N R C Research Press
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/67513 https://doi.org/10.1139/E10-091 https://openresearch-repository.anu.edu.au/bitstream/1885/67513/5/01_Amelin_Evolution_of_early_crust_in_2011.pdf.jpg |
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 - |
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