2001 (v1)
Publication
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S
M
SCAMBELLURI , Marco
Last name: SCAMBELLURI
First name: Marco
Email: marco.scambelluri@unige.it
Institution: UOM
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2011 (v1)Publication
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2004 (v1)Publication
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2013 (v1)Publication
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1992 (v1)Publication
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2002 (v1)Publication
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2001 (v1)Publication
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1991 (v1)Publication
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1988 (v1)Publication
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2004 (v1)Publication
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1987 (v1)Publication
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1997 (v1)Publication
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1997 (v1)Publication
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1999 (v1)PublicationMg-metasomatism of oceanic gabbros and its control on Ti-clinohumite formation during eclogitization
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1994 (v1)Publication
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2011 (v1)Publication
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1994 (v1)Publication
In: Compagnoni R. e Messiga B. (eds.), Guide-book to the field excursion B1 "High pressure metamorphism in the Western Alps". 16th General Meeting of the International Mineralogical Association
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2003 (v1)Publication
U-Pb geochronology with ion microprobe (SHRIMP) analysis has been carried out on eclogite-facies rocks of the Beigua Unit, an ophiolitic slice of the Voltri Massif, Western Alps. The investigated samples are eclogites and high-pressure metasomatic rocks (metarodingites and centimetre-sized Ti-clinohumite-bearing dykes). Zircon contained in an...
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1996 (v1)Publication
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2011 (v1)Publication
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1993 (v1)Publication
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2012 (v1)Publication
Serpentinites formed by alteration of oceanic and forearc mantle are major volatile and fl uid-mobile element reservoirs for arc magmatism, though direct proof of their dominance in the subduction-zone volatile cycles has been elusive. Boron isotopes are established markers of fl uid-mediated mass transfer during subduction. Altered oceanic...
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2004 (v1)Publication
We discuss some aspects of the release of light elements and volatile components during subduction of serpentinite and metasedimentary systems. Enrichment in B, CI, and Sr during serpentinization of the oceanic mantle is followed by their progressive release in the subduction fluids. Olivine-orthopyroxene rocks formed after significant...
Uploaded on: April 14, 2023