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Chaput M., Pinel Virginie, Famin V., Michon L., Froger J. L. (2014). Cointrusive shear displacement by sill intrusion in a detachment : a numerical approach. Geophysical Research Letters, 41 (6), p. 1937-1943. ISSN 0094-8276.

Titre du document
Cointrusive shear displacement by sill intrusion in a detachment : a numerical approach
Année de publication
2014
Type de document
Article référencé dans le Web of Science WOS:000334264900017
Auteurs
Chaput M., Pinel Virginie, Famin V., Michon L., Froger J. L.
Source
Geophysical Research Letters, 2014, 41 (6), p. 1937-1943 ISSN 0094-8276
Sheared sills are observed at Piton des Neiges (the eroded basaltic volcano of La Reunion) and are a suspected cause of the coeruptive flank displacement of Piton de la Fournaise in 2007. We performed a 2-D numerical study to quantify the perturbation induced by sill injection within a volcanic edifice. Magma is considered as an inviscid and pressurized fluid injected in an initially stable edifice under gravity-controlled extension. Two cases of injection are tested, in an elastic homogeneous edifice or along a detachment controlled by a friction law. We show that sill injection induces tangential displacements. This effect is strongly increased when sills are emplaced along a detachment, producing extension behind the injection and potentially ending in a large-scale flank collapse. Sill injections can thus explain the cointrusive shear deformation observed at Piton des Neiges and the tangential displacements measured at Piton de la Fournaise in 2007.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Géophysique interne [066]
Description Géographique
REUNION
Localisation
Fonds IRD [F B010061953]
Identifiant IRD
fdi:010061953
Contact