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Rockmagnetic and paleomagnetic study of historical lava flows from Mt. Etna (Sicily, Italy)

dc.contributor.authorCalvo, M.
dc.contributor.authorPerrin, M.
dc.contributor.authorPrévot, M.
dc.date.accessioned2016-10-10T09:39:10Z
dc.date.available2016-10-10T09:39:10Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12737
dc.description.abstract70 basaltic lava flows from Mt. Etna erupted in 1910, 1928, 1950 and 1979 were sampled to carry out rockmagnetic studies In order to determine their magnetic mineralogy and paleomagnetic stability and to asses their suitability for paleointensity studies. Rockmagnetic studies included measurement of susceptibility versus temperature curves, vibrating sample thermomagnetometer experiments, measurement of isothermal remanence acquisition curves and determination of viscosity index V. Three different types of susceptibility versus temperature curves allowed to recognize magnetite, ilmeno-hematite and/or oxidized low-Ti titanomagnetite as main ferromagnetic phases. In some samples a fraction of grains with multidomain structure could be recognized. Nevertheless, the main part of the studied samples showed a viscosity index V<5%.A paleomagnetic study carried out on a lava flow from 1689 in order to obtain additional data for a secular variation curve for Sicily yielded the following result: D= 344.6, 1= 64.2, N=14, cc95 = 1.5 and k=737en_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherRock magnetismen_US
dc.subject.otherPaleointensityen_US
dc.subject.otherSecular variationen_US
dc.subject.otherMt. Etnaen_US
dc.titleEstudio magnético y paleomagnético de coladas históricas del Etna (Sicilia, Italia)en_US
dc.titleRockmagnetic and paleomagnetic study of historical lava flows from Mt. Etna (Sicily, Italy)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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