The transition from endogenous to exogenous growth of lava domes with the development of shear bands

Journal of Volcanology and Geothermal Research

Volumn 171, Issue 3-4, 2008, Pages 237-257

  Hale, Alina J ^a   Wadge, Geoff ^b  

^a UNIVERSITY OF QUEENSLAND   (Australia)

^b UNIVERSITY OF READING   (United Kingdom)

Author keywords

computational model; Finite Element Method; lava dome; shear bands; Soufri re Hills Volcano

Indexed keywords

BRITTLENESS; COMPUTATIONAL METHODS; COMPUTER SIMULATION; MATHEMATICAL MODELS; RHEOLOGY; SEDIMENT TRANSPORT; SHEAR BANDS; SHEAR STRESS; VISCOSITY; VOLCANIC ROCKS;

LAVA DOMES; MAGMA EXTRUSION RATE;

VOLCANOES;

ENDOGENOUS GROWTH; EXTRUSION; FINITE ELEMENT METHOD; FORMATION MECHANISM; LAVA DOME; LAVA FLOW; RHEOLOGY; SHEAR BAND; SHEAR STRESS;

ATLANTIC ISLANDS; ATLANTIC OCEAN; CARIBBEAN ISLANDS; LEEWARD ISLANDS [LESSER ANTILLES]; LESSER ANTILLES; MONTSERRAT; SOUFRIERE HILLS VOLCANO;

EID: 41849090793     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2007.12.016     Document Type: Article

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