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Transmogrification of ocean into continent: implications for continental evolution
When continents collide, the typical embayments and protrusions along their rifted margins make it likely that fragments of seafloor will be trapped within the growing orogenic belt. These trapped seafloor fragments become preferential depocenters for marine and terrestrial sedimentation. After ∼0.5...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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National Academy of Sciences
2022
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9169811/ https://www.ncbi.nlm.nih.gov/pubmed/35377785 http://dx.doi.org/10.1073/pnas.2122694119 |