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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: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:scopusPyroclastic dune bedforms: macroscale structures and lateral variations. Examples from the 2006 pyroclastic currents at Tungurahua (Ecuador)
ArticleAbstract: Pyroclastic currents are catastrophic flows of gas and particles triggered by explosive volcanic eruPalabras claves:Backset lamination, dune bedforms, pyroclastic currents, stoss-aggradation, TungurahuaAutores:Bouysson M., Chaffaut Q., Dingwell D.B., Douillet G.A., Gegg L., Hoelscher I., Julien Bernard, Kueppers U., Mato C., Ritz V.A., Schlunegger F., Witting P.Fuentes:googlescopus