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Water saturation of hydrothermal smectite-rich clay might have promoted slope instability prior the 1998 debris avalanche at casito volcano, Nicaragua

Bibliographic reference Delmelle, Pierre ; Opfergelt, Sophie ; Boivin, P ; Delvaux, Bruno. Water saturation of hydrothermal smectite-rich clay might have promoted slope instability prior the 1998 debris avalanche at casito volcano, Nicaragua.AGU Fall Meeting (San Francisco, USA, du 11/12/2006 au 15/12/2006). In: EOS Trans. AGU, Fall Meet. Suppl., Vol. 87, no. 52, p. T13D-0546 (2006)
Permanent URL http://hdl.handle.net/2078.1/73282