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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5401

Authors: Hautmann, S.*
Gottsmann, J.*
Sparks, R. S. J.*
Costa, A.*
Melnik, O.*
Voight, B.*
Title: Modelling ground deformation caused by oscillating overpressure in a dyke conduit at Soufrière Hills Volcano, Montserrat
Title of journal: Tectonophysics
Series/Report no.: /471 (2009)
Publisher: Elsevier
Issue Date: 2009
DOI: 10.1016/j.tecto.2008.10.021
Keywords: Soufrière Hills Volcano
Dyke conduit
Finite Element Model
Ground deformation
Abstract: A dyke conduit has been shown to be a realistic model for the shallow magmatic feeder system for the dome forming eruption at Soufrière Hills Volcano, Montserrat. Here we use a three-dimensional Finite Element model to examine the ground deformation that can be expected due to the pressurization of a dyke conduit. We find that the generated deformation has a bilateral symmetry with nearly no displacement in the direction of dyke strike, and a maximal ground deformation about 1 km away from the vent in the perpendicular direction. Resultant surface deformation is mainly triggered by the upper part of the feeder system, where the dyke opens into a cylindrical conduit. We apply our deformation model to investigate tilt data collected in 1997 in order to infer the orientation of the dyke. We obtain a best-fit for a NNW–SSE trending dyke, which matches observations of the ground displacement field obtained by differential GPS and the alignment of main structural geologic features of southern Montserrat.
Appears in Collections:04.07.08. Volcanic arcs
Papers Published / Papers in press
05.01.03. Inverse methods
04.08.08. Volcanic risk

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