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Episodic zircon age spectra of orogenic granitoids: The supercontinent connection and continental growth
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“were correlated with continental growth and supercontinent formation (Condie and Aster, 2010).”
BackgroundWhy Archaean TTG cannot be generated by MORB melting in subduction zones
Martin, H., Moyen, J.-F., Guitreau, M., Blichert-Toft, J., & Le Pennec, J.-L. (2014) · Lithos · doi:10.1016/j.lithos.2014.02.017 · Cited by 346
Metadata
- Authors
- Condie, K. C., & Aster, R. C.
- Venue
- Precambrian Research
- Publisher
- Elsevier BV
- Published
- 2010-07
- Volume
- 180
- Issue
- 3-4
- Pages
- 227-236
- ISSN
- 0301-9268 (ISSN-L)
- OpenAlex
- W1973876227
- Cited by
- 490
- References
- 2
- FWCI
- 18.37
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.elsevier.com/tdm/userlicense/1.0/ (tdm)
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- Condie, K. C., & Aster, R. C. (2010). Episodic zircon age spectra of orogenic granitoids: The supercontinent connection and continental growth. Precambrian Research. https://doi.org/10.1016/j.precamres.2010.03.008
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