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Forty years of TTG research
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Cited by
Laurent, O., Martin, H., Moyen, J. F., & Doucelance, R. (2014) · Lithos · doi:10.1016/j.lithos.2014.06.012 · Cited by 938
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Secular change and the onset of plate tectonics on Earth
Palin, R. M., Santosh, M., Cao, W., Li, S.-S., Hernández-Uribe, D., & Parsons, A. (2020) · Earth-Science Reviews · doi:10.1016/j.earscirev.2020.103172 · Cited by 355
“…of a hot Archean mantle have demonstrated that oceanic lithosphere was too buoyant to subduct (Van Hunen and van den Berg, 2008; van Hunen and Moyen, 2012), whereas oceanic lithosphere formed from a relatively cool Archean mantle would have a larger density and viscosity contrast across the…”
BackgroundInfluentialWhy 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
Self-citationGeneration of felsic crust in the Archean: A geodynamic modeling perspective
Sizova, E., Gerya, T., Stüwe, K., & Brown, M. (2015) · Precambrian Research · doi:10.1016/j.precamres.2015.10.005 · Cited by 332
Metadata
- Authors
- Moyen, J.-F., & Martin, H.
- Venue
- Lithos
- Publisher
- Elsevier BV
- Published
- 2012-09
- Volume
- 148
- Pages
- 312-336
- ISSN
- 0024-4937 (ISSN-L)
- OpenAlex
- W2055172418
- Cited by
- 1,015
- References
- 252
- FWCI
- 52.04
- Type
- journal article
- Language
- en
- Open access
- closed
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