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↑ Hautmann et al. (2014), Strain field analysis on Montserrat (W.I.) as a tool for assessing permeable flow paths in the magmatic system of Soufrière Hills Volcano, Geochemistry, Geophysics, Geosystems vol. 15 p676-690
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↑ Burton et al. (2007) Magmatic Gas Composition Reveals the Source Depth of Slug-Driven Strombolian Explosive Activity Science vol 317 p.227-230.
↑ Royal Society Climate Change Controversies, London, June 2007
