Tracking the permeable porous network during strain-dependent magmatic flow

Journal of Volcanology and Geothermal Research

Volumn 260, Issue , 2013, Pages 117-126

  Kendrick, J E ^a,b   Lavallee Y ^a,b   Hess, K U ^a   Heap, M J ^c   Gaunt, H E ^d   Meredith, P G ^d   Dingwell, D B ^a  

^a UNIVERSITY OF MUNICH   (Germany)

^b UNIVERSITY OF LIVERPOOL   (United Kingdom)

^c UNIVERSITÉ DE STRASBOURG EOST   (France)

^d UNIVERSITY COLLEGE LONDON   (United Kingdom)

Author keywords

Damage; Deformation; Magma; Rheology; Strain localization; Viscosity

Indexed keywords

DAMAGE; DYNAMIC POISSON'S RATIOS; DYNAMIC YOUNG'S MODULUS; MAGMA; MAXIMUM PRINCIPAL STRESS; MECHANICAL DEGRADATION; SIGNIFICANT DIFFERENCES; STRAIN LOCALIZATIONS;

CEMENTS; COALESCENCE; COMPLEX NETWORKS; DEFORMATION; DOMES; ELASTIC MODULI; ELASTICITY; NON NEWTONIAN LIQUIDS; POROSITY; RHEOLOGY; VISCOSITY; VOLCANOES;

STRAIN RATE;

DEFORMATION MECHANISM; EXPLOSIVE VOLCANISM; LAVA DOME; MAGMATISM; NON-NEWTONIAN FLUID; POISSON RATIO; POROSITY; RHEOLOGY; STRESS-STRAIN RELATIONSHIP; VISCOELASTICITY; VOID RATIO; VOLCANIC ERUPTION; VOLCANOLOGY; YOUNG MODULUS;

COLIMA; COLIMA VOLCANO; MEXICO [NORTH AMERICA];

EID: 84880293816     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2013.05.012     Document Type: Article

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