Weibull-distributed dyke thickness reflects probabilistic character of host-rock strength

Magmatic sheet intrusions (dykes) constitute the main form of magma transport in the Earth’s crust. The size distribution of dykes is a crucial parameter that controls volcanic surface deformation and eruption rates and is required to realistically model volcano deformation for eruption forecasting....

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Detalles Bibliográficos
Autores principales: Krumbholz, Michael, Hieronymus, Christoph F., Burchardt, Steffi, Troll, Valentin R., Tanner, David C., Friese, Nadine
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3926007/
https://www.ncbi.nlm.nih.gov/pubmed/24513695
http://dx.doi.org/10.1038/ncomms4272

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3926007/
https://www.ncbi.nlm.nih.gov/pubmed/24513695
http://dx.doi.org/10.1038/ncomms4272

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