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Rift migration explains continental margin asymmetry and crustal hyper-extension
When continents break apart, continental crust and lithosphere are thinned until break-up is achieved and an oceanic basin is formed. The most remarkable and least understood structures associated with this process are up to 200 km wide areas of hyper-extended continental crust, which are partitione...
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| Main Authors: | , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Pub. Group
2014
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4059923/ https://ncbi.nlm.nih.gov/pubmed/24905463 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms5014 |
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