Dike intrusions during rifting episodes obey scaling relationships similar to earthquakes

As continental rifts evolve towards mid-ocean ridges, strain is accommodated by repeated episodes of faulting and magmatism. Discrete rifting episodes have been observed along two subaerial divergent plate boundaries, the Krafla segment of the Northern Volcanic Rift Zone in Iceland and the Manda-Har...

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Detalles Bibliográficos
Autores principales: L., Passarelli, E., Rivalta, A., Shuler
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3904149/
https://www.ncbi.nlm.nih.gov/pubmed/24469260
http://dx.doi.org/10.1038/srep03886

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3904149/
https://www.ncbi.nlm.nih.gov/pubmed/24469260
http://dx.doi.org/10.1038/srep03886

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