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Tracking the permeable porous network during strain-dependent magmatic flow
ArticleAbstract: Rheological variations have been postulated as the cause of transitions from effusive to explosive vPalabras claves:damage, Deformation, Magma, rheology, Strain localization, ViscosityAutores:Dingwell D.B., Elizabeth H. Gaunt, Heap M.J., Hess K.U., Kendrick J.E., Lavallée Y., Mebkp_redith P.G.Fuentes:scopusSedimentology and geomorphology of the deposits from the August 2006 pyroclastic density currents at Tungurahua volcano, Ecuador
ArticleAbstract: The deposits of the pyroclastic density currents from the August 2006 eruption of Tungurahua show thPalabras claves:Flow stripping, Hydraulic jump, Pyroclastic density currents, Sedimentary wedge, TungurahuaAutores:Claude Robin, Daniel Alejandro Pacheco, Dingwell D.B., Douillet G.A., Goldstein F., Hall M.L., Hanson J.B., Jorge Eduardo Bustillos, Kueppers U., Lavallée Y., Letort J., Patricio A. Ramón, Tsang-Hin-Sun E., Von Aulock F.Fuentes:scopusSeismogenic frictional melting in the magmatic column
ArticleAbstract: Lava dome eruptions subjected to high extrusion rates commonly evolve from endogenous to exogenous gPalabras claves:Autores:De Angelis S., Dingwell D.B., Elizabeth H. Gaunt, Ferk A., Hess K.U., Kendrick J.E., Lavallée Y., Leonhardt R., Mebkp_redith P.G.Fuentes:scopus