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Mantle exhumation at magma-poor rifted margins controlled by frictional shear zones
The transition zone from continental crust to the mature mid-ocean ridge spreading center of the Iberia-Newfoundland magma-poor rifted margins is mostly composed of exhumed mantle characterized by highs and domes with varying elevation, spacing and shape. The mechanism controlling strain localizatio...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2022
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8960832/ https://www.ncbi.nlm.nih.gov/pubmed/35347122 http://dx.doi.org/10.1038/s41467-022-29058-1 |