Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4556
AuthorsLandi, P.* 
Métrich, N.* 
Bertagnini, A.* 
Rosi, M.* 
TitleRecicling and “re-hydration” of degassed magma inducing transient dissolution/crystallization events at Stromboli (Italy)
Issue Date10-Jul-2008
Series/Report no./174 (2008)
DOI10.1016/j.jvolgeores.2008.02.013
URIhttp://hdl.handle.net/2122/4556
Keywordsmineral dissolution
magma chemistry
volatiles
trace elements
Stromboli
Subject Classification04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology 
04. Solid Earth::04.08. Volcanology::04.08.03. Magmas 
04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk 
AbstractIntrusive degassing and recycling of degassed and dense magma at depth have been proposed for a long time at Stromboli. The brief explosive event that occurred at the summit craters on 9 January 2005 threw out bombs and lapilli that could be good candidates to illustrate recycling of shallow degassed magma at depth. We present an extensive data set on both the textures and the mineral, bulk rock and glassy matrix chemistry of the “9 Jan” products. The latter have the common shoshonitic–basaltic bulk composition of lavas and scoriae issued from typical strombolian activity. In contrast they differ by the heterogeneous chemistry of their matrix glasses and their crystal textures that testify to crystal dissolution event(s) just prior magma crystallization upon ascent and eruption. Comparison between mineral paragenesis of the natural products and experimental phase equilibria suggest water-induced magma re-equilibration. We propose that mineral dissolution is related to water enrichment of the recycled degassed magma, via differential gas bubble transfer and to some extents its physical mixing with volatile-rich magma blobs. However, all these features illustrate transient processes. Even though evidence of mineral dissolution is ubiquitous at Stromboli, its effect on the bulk magma chemistry is minor because of the subtle interplay between mineral dissolution and crystallization in magmas having comparable bulk chemistry.
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