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The initial break-up of Pangæa elicited by Late Palæozoic deglaciation
The break-up of Pangæa was principally facilitated by tensional plate stress acting on pre-existing suture zones. The rifting of Pangæa began during the Early Permian along the southern Tethys margin and produced the lenticular-shaped continent known as Cimmeria. A mantle-plume model is ascribed to...
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| Publicado no: | Sci Rep |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group
2016
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4980595/ https://ncbi.nlm.nih.gov/pubmed/27511791 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep31442 |
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