Why Archaean TTG cannot be generated by MORB melting in subduction zones
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TTG gneisses are typically interpreted as formed through partial melting of amphibolite or eclogite due to drip tectonics or subduction of oceanic plateaus.
“The volumetrically dominant lithology in Archean terranes -TTG gneissesis typically interpreted as formed through partial melting of amphibolite or eclogite due to drip tectonics (Nebel et al., 2018) or subduction of oceanic plateaus (e.g.Martin et al., 2014;Hastie et al., 2016).”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Martin et al., 2014
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“…is stable up to ~10 GPa and may so carry H2O and other trace elements (REE, Sr, Th, and U) into the mantle more effectively than other hydrous phases, such as amphibole, epidote, and chlorite (Pawley, 1994; Schmidt and Poli, 1998; Spandler et al., 2003; Usui et al., 2007; Martin et al., 2014).”
BackgroundGeneration of felsic crust in the Archean: A geodynamic modeling perspective
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- Authors
- Martin, H., Moyen, J.-F., Guitreau, M., Blichert-Toft, J., & Le Pennec, J.-L.
- Affiliations
- Centre National de la Recherche Scientifique (FR)
- University of New Hampshire (US)
- Corresponding author
- Martin, Hervé
- Venue
- Lithos
- Publisher
- Elsevier BV
- Published
- 2014-06
- Volume
- 198-199
- Pages
- 1-13
- ISSN
- 0024-4937 (ISSN-L)
- OpenAlex
- W2042986233
- Cited by
- 346
- References
- 107
- Citations by year
- 2026: 29 · 2025: 24 · 2024: 27 · 2023: 23 · 2022: 34 · 2021: 35 · 2020: 46 · 2019: 30 · 2018: 22 · 2017: 24 · 2016: 32 · 2015: 16 · 2014: 4
- FWCI
- 22.54
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Lithos (publishedVersion)
- HAL (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
- Keywords
- tonalite-trondhjemite-granodiorite, subduction zone, oceanic plateau, mantle plume, Carnegie Ridge, Galapagos hotspot, Iceland mantle plume, crustal growth
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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