'Wet' low angle subduction: a possible mechanism below the Tanzania craton 2Ga ago
The hypothesis that much of the lithosphere of the Archaean Tanzania Craton was hydrated, by the dehydration of a buoyant subduction 2Ga ago is presented in this study. Buoyant subduction is a potential mechanism for thermal erosion and metasomatism of extensive regions of the cold overlying contine...
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| Veröffentlicht in: | Mineralogy and petrology 2009-05, Vol.96 (1-2), p.113-120 |
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| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
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