Archaean fluid-assisted crustal cannibalism recorded by low δ 18 O and negative ε Hf(T) isotopic signatures of West Greenland granite zircon
The role of fluids during Archaean intra-crustal magmatism has been investigated via integrated SHRIMP U-Pb, δ18O and LA-MC-ICPMS 176Hf isotopic zircon analysis. Six rock samples studied are all from the Nuuk region (southern West Greenland) including tw
Published in: | Contributions to Mineralogy and Petrology |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Springer
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/19481 https://doi.org/10.1007/s00410-010-0578-z https://openresearch-repository.anu.edu.au/bitstream/1885/19481/7/C1-10-Archaean_fluid-assisted_crustal_cannibalism.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/19481/9/Hiess_et_al.%252C_2010.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/19481/11/01_Hiess_Archaean_fluid-assisted_2011.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/19481/13/02_Hiess_Archaean_fluid-assisted_2011.pdf.jpg |
Summary: | The role of fluids during Archaean intra-crustal magmatism has been investigated via integrated SHRIMP U-Pb, δ18O and LA-MC-ICPMS 176Hf isotopic zircon analysis. Six rock samples studied are all from the Nuuk region (southern West Greenland) including tw |
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