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Regulating continent growth and composition by chemical weathering
Continents ride high above the ocean floor because they are underlain by thick, low-density, Si-rich, and Mg-poor crust. However, the parental magmas of continents were basaltic, which means they must have lost Mg relative to Si during their maturation into continents. Igneous differentiation follow...
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| Autors principals: | , , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2008
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2278177/ https://ncbi.nlm.nih.gov/pubmed/18362343 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0711143105 |
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