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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2017
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5653657/ https://www.ncbi.nlm.nih.gov/pubmed/29062023 http://dx.doi.org/10.1038/s41467-017-01256-2 |