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  Oral 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:

Monday, 25 April 2005

Lecture Room: Lecture Room 24

Chairperson: CLEMENS, J.

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10:30 - 10:45
EGU05-A-06446;  VGP29-1MO2O-001
Pascual, E.; Pin, Ch.; Donaire, T.
Geochemical tools in discriminating rival petrogenetic processes in granitoid suites: a case on the Los Pedroches Batholith, Iberian Massif, Spain

10:45 - 11:00
EGU05-A-03500;  VGP29-1MO2O-002
Helps, P. A.; Clemens, J. D.; Petford, N.
Source-related chemical and isotopic heterogeneities in granitoids

11:00 - 11:15
EGU05-A-03533;  VGP29-1MO2O-003
Clemens, J. D.; Darbyshire, D.; Flinders, J.
Multiple magmatic lineages in calcalkaline spatially and temporally related granitoid suites: the example of the Arrochar and Garabal Hill-Glen Fyne intrusions of Scotland

11:15 - 11:30
EGU05-A-09213;  VGP29-1MO2O-004
Hogan, J. P.
Geochemical variability within “closed system” granites – a consequence of incremental assembly of granite plutons and batholiths (solicited)

11:30 - 11:45
EGU05-A-04915;  VGP29-1MO2O-005
Dupont, A.; Vander Auwera, J.; Pin, C.; Paquette, J.-L.; Bogaerts, M.
Inefficiency of magma mixing and source heterogeneity in the genesis of granitoids : the example of the Farsund intrusion (southern Norway)

11:45 - 12:00
EGU05-A-00846;  VGP29-1MO2O-006
Martin, E.; Sigmarsson, O.
Implication for the origin of tholeiitic silicic magmas from atmospheric pressure fractional crystallization of basaltic lava flows on Reykjanes peninsula (Iceland), Lanzarote (Canary Islands) and Masaya (Nicaragua).

12:00
END OF SESSION




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