Water saturation of hydrothermal smectite-rich clay might have promoted slope instability prior the 1998 debris avalanche at casito volcano, Nicaragua
(2006) AGU Fall Meeting — Location: San Francisco, USA (11.December.2006)
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University of Oxford, Uk
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Delmelle, P., Opfergelt, S., Boivin, P., & Delvaux, B. (2006). Water saturation of hydrothermal smectite-rich clay might have promoted slope instability prior the 1998 debris avalanche at casito volcano, Nicaragua. EOS Trans. AGU, Fall Meet. Suppl., 87(52), T13D-0546. https://hdl.handle.net/2078.5/151285 (Original work published 2006)