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The effect of giant lateral collapses on magma pathways and the location of volcanism
Flank instability and lateral collapse are recurrent processes during the structural evolution of volcanic edifices, and they affect and are affected by magmatic activity. It is known that dyke intrusions have the potential to destabilise the flanks of a volcano, and that lateral collapses may chang...
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| Publicado no: | Nat Commun |
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| Main Authors: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5653657/ https://ncbi.nlm.nih.gov/pubmed/29062023 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-017-01256-2 |
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