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4.2 Ga zircon xenocryst in an Acasta gneiss from northwestern Canada: Evidence for early continental crust
Tsuyoshi Iizuka
Tsuyoshi Iizuka
1
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Ookayama Meguro-ku, Tokyo 152-8551, Japan
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Kenji Horie
Kenji Horie
2
Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan
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Tsuyoshi Komiya
Tsuyoshi Komiya
3
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Ookayama Meguro-ku, Tokyo 152-8551, Japan
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Shigenori Maruyama
Shigenori Maruyama
3
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Ookayama Meguro-ku, Tokyo 152-8551, Japan
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Takafumi Hirata
Takafumi Hirata
3
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Ookayama Meguro-ku, Tokyo 152-8551, Japan
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Hiroshi Hidaka
Hiroshi Hidaka
4
Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan
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Brian F. Windley
Brian F. Windley
5
Department of Geology, University of Leicester, Leicester LE1 7RH, UK
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Geology (2006) 34 (4): 245-248.
Published:
April 01, 2006
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Tsuyoshi Iizuka, Kenji Horie, Tsuyoshi Komiya, Shigenori Maruyama, Takafumi Hirata, Hiroshi Hidaka, Brian F. Windley; 4.2 Ga zircon xenocryst in an Acasta gneiss from northwestern Canada: Evidence for early continental crust. Geology ; 34 (4): 245–248. doi: https://doi.org/10.1130/G22124.1
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Index Terms/Descriptors
- absolute age
- Archean
- Canada
- cathodoluminescence
- continental crust
- crust
- dates
- experimental studies
- geochemistry
- gneisses
- Hadean
- high-resolution methods
- ICP mass spectra
- ion probe data
- laser ablation
- laser methods
- mass spectra
- metamorphic rocks
- nesosilicates
- Northwest Territories
- orthosilicates
- Paleoarchean
- Precambrian
- reworking
- silicates
- spectra
- trace elements
- U/Pb
- Western Canada
- xenocrysts
- zircon
- zircon group
- Acasta Gneiss
Latitude & Longitude
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