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  Poster Programme - VGP29 Elemental and isotopic variations within felsic magmas: do we know the causes?

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Convener: Clemens, J.
Co-Convener: Finger, F.
Co-Sponsorship:


Author in Attendance:

Monday, 25 April 2005 17:30 - 19:00
Display Time: Monday, 25 April 2005 08:00 -
Monday, 25 April 2005 19:00
Poster Area: Foyer A

Chairperson: HELPS, P. A.

Select complete timeblock
A157
EGU05-A-05667;  VGP29-1MO5P-0157
Gagnevin, D.; Daly, J.S.; Poli, G.; Morgan, D.; Waight, T.E.
Trace element, Sr and Pb isotopic zoning in K-feldspar megacrysts from the Monte Capanne monzogranite (Elba, Italy): evidence for a multi-stage crystallization history

A158
EGU05-A-09741;  VGP29-1MO5P-0158
Acosta-Vigil, A.; Cesare, B.; London, D.; Morgan VI, G. B.
The composition of melt during crustal anatexis from the analysis of silicate glass within extruded migmatitic enclaves in el Hoyazo dacites, SE Spain

A159
EGU05-A-05409;  VGP29-1MO5P-0159
Pupier, E.; Barbey, P.; Toplis, M.J.; Bussy, F.; Pons, P.
To what extent are granites representative of melt?

A160
EGU05-A-07224;  VGP29-1MO5P-0160
Cabato, MEJA; Altherr, R.; Ludwig, T.
Li, Be, B in dacites from Nea Kameni, Santorini Caldera (Greece)

A161
EGU05-A-09497;  VGP29-1MO5P-0161
Piochi, M.
Magma compositions at the Somma-Vesuvius (Italy): open problems and new interpretation approaching to a possible resolution

A162
EGU05-A-01935;  VGP29-1MO5P-0162
Clemens, J. D.; Helps, P. A.; Stevens, G.
Chemical variations in granitic magmas: source-inherited or products of magmatic processes?

A163
EGU05-A-07465;  VGP29-1MO5P-0163
Volkova, E.V.; Syritso, L.F.
Conditions of geochemical specialization of rare-metal granites by the example of Eastern Transbaikalia

A164
EGU05-A-06756;  VGP29-1MO5P-0164
Syritso, L.F.; Abushkevich, V.S.; Levsky, L.K.; Badanina, E.V.
On the nature of mantle component in isotope systems of rare-metal granites

A165
EGU05-A-04381;  VGP29-1MO5P-0165
Paone, A.
Petrogenesis of Trachyte and Rhyolite Magmas on Ponza Island (Italy) and its Relationship to the Campanian Magmatism




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