Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4495
Authors: Dini, A.* 
Mazzarini, F.* 
Musumeci, G.* 
Rocchi, S.* 
Title: Multiple hydro-fracturing by boron-rich fluids in the Late Miocene contact aureole of eastern Elba Island (Tuscany, Italy)
Journal: Terra Nova 
Series/Report no.: 4/20 (2008)
Publisher: Blackwell Publishing Ltd
Issue Date: Aug-2008
DOI: 10.1111/j.1365.3121.2008.00823.x
URL: http://www3.interscience.wiley.com/cgi-bin/fulltext/120840284/PDFSTART
Keywords: Hydro-fractures
geothermal systems
Magmatism
southern Tuscany
Subject Classification04. Solid Earth::04.01. Earth Interior::04.01.99. General or miscellaneous 
04. Solid Earth::04.04. Geology::04.04.09. Structural geology 
Abstract: In eastern Elba Island (Tuscany, Italy), a shallow crustal level felsic, tourmaline-bearing, dyke-sill swarm of Late Miocene age is associated with abundant tourmaline-quartz hydrothermal veins and metasomatic masses. Development of these veins and masses in the host rocks demonstrates multiple hydro-fracturing by magmatic, boron-rich saline fluid. Tourmalines in felsic dykes are schorl, whereas in veins and metasomatic masses, tourmaline composition ranges from schorl-dravite through dravite to uvite. This compositional shift is evidence for an increasing contribution to the magmatic boron-rich fluids by a Mg-Ca-Ti-rich external component represented by biotite-rich and amphibolite host rocks. This system can be envisaged as an exposed proxy of the high temperature hydrothermal system presently active in the deepest part of the Larderello-Travale geothermal field (Tuscany).
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