EGU General Assembly 2008
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  Poster Programme - SM6 The European Lithosphere: What do we know? (co-listed in TS; co-sponsored by ILP Task Force)

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Convener: Artemieva, I.
Co-Convener: Garrido, C., Cloetingh, S., Coltorti, M., Tommasi, A., Szabo, C.
Co-Sponsorship: ILP Task Force

Author in Attendance:

Thursday, 17 April 2008 17:30 - 19:00
Display Time: Thursday, 17 April 2008 08:00 -
Thursday, 17 April 2008 19:30
Poster Area: Hall A

Chairperson: TOMMASI A, SZABO C

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EGU2008-A-08761;  SM6-1TH5P-0504
Artemieva, I M; Thybo, H
Deep Norden: Highlights of the lithospheric structure of Northern Europe, Iceland, and Greenland

EGU2008-A-08813;  SM6-1TH5P-0505
Artemieva, I M; Thybo, H; Kaban, M K
Deep Europe: Highlights of the lithospheric structure from multidisciplinary geophysical data

EGU2008-A-02441;  SM6-1TH5P-0506
Sodoudi, F.; Geissler, W. H.; Kind, R.
The thickness of the European Lithosphere as seen by S receiver functions

EGU2008-A-02435;  SM6-1TH5P-0507
Le Roux, V.; Bodinier, J.-L.; Alard, O.; O'Reilly, S.Y.; Tommasi, A.; Vauchez, A.
The Lherz massif: 2 Ga history of mantle evolution

EGU2008-A-03203;  SM6-1TH5P-0508
Demetrescu, C.; Tumanian, M.
Thermal and rheological models of the Carpathians foreland on the Romanian territory, constrained by seismic velocity data

EGU2008-A-03285;  SM6-1TH5P-0509
Dobrica, V.; Tumanian, M.
Improved thermal model simulating the Neogene volcanic process in Harghita Mountains (East Carpathians)

EGU2008-A-00633;  SM6-1TH5P-0510
Nédli, Zs.; Princivalle, F.; Downes, H. ; Dégi, J.; Szabó, Cs.
Petrology and thermobarometry of mantle xenoliths from the Poiana Rusca (W Romania)

EGU2008-A-07333;  SM6-1TH5P-0511
Kovacs, I; Falus, Gy; Hidas, K.; Szabo, Cs.
Collision induced astenospheric flow in the Carpathian Pannonian region: a new interpretation for Cenozoic geodynamics???

EGU2008-A-04690;  SM6-1TH5P-0512
Dando, B. D.; Houseman, G. A.; Stuart, G. W.
Seismic imaging of the Vienna and western Pannonian basins

EGU2008-A-05285;  SM6-1TH5P-0513
Hausmann, H.; Hoyer, S.; Zeisz, K.; Schurr, B.; Brückl, E.; CBP Team, .; ALPASS Team, .
Seismicity of the Vienna Basin from the temporary ALPASS and CBP deployments

EGU2008-A-10151;  SM6-1TH5P-0514
Behm, M.; Lippitsch, R.; Kissling, E.; Brückl, E.; Grad, M.; Sumanovac, F.
A new Moho map for the entire Alpine region

EGU2008-A-10212;  SM6-1TH5P-0515
Jiménez-Munt, I.; Fernàndez, M.; Vergés, J.; Zeyen, H.; Fullea, J.; Afonso , J.C.; García-Castellanos, D.
The lithospheric structure across the NW Moroccan Margin: evidences for large scale tectonic inversion

EGU2008-A-07386;  SM6-1TH5P-0516
France, L; Chazot, G; Kornprobst, J; Dallai, L; Vannucci, R; Bosq, C
Petrological and geochemical study of late-orogenic mantle garnet pyroxenites. Implications on magmatism in old orogenic regions.

EGU2008-A-09040;  SM6-1TH5P-0517
Matusiak, M; Grégoire, M; Puziewicz, J
Petrology of mantle beneath Central Europe: a case study of the Lutynia (Sudetes, SW Poland) peridotite xenoliths

EGU2008-A-06067;  SM6-1TH5P-0518
Atanasiu, L.; Besutiu, L.
Gravity-based models of the northern Moesian Plate

EGU2008-A-06654;  SM6-1TH5P-0519
Marello, L.; Ebbing, J.; Ritzmann, O.
A new 3D regional density model for the Barents Sea Region

EGU2008-A-03821;  SM6-1TH5P-0521
Eken, T.; Plomerova, J.; Roberts, R.; Shomali, H.; Vecsey, L.; Babuska, V.; Bodvarsson, R.
Does Baltic Shield mantle anisotropy in Sweden resemble the fabric of the Archean-Proterozoic domains in central Finland?

EGU2008-A-06798;  SM6-1TH5P-0522
Bogdanova, S.V.; Starostenko, V.I.; Gintov, O.B.; Pashkevich, I.K.; Kuprienko, P.Ya.; Kutas, R.Ya.; Makarenko, I.V.; Tsvetkova, T.A.
Long-lived E-W fault zones in the lithosphere of western Sarmatia

EGU2008-A-05598;  SM6-1TH5P-0523
Plotnikova, I.N.
Influence of Deep Processes in the Lithosphere on Features of Development of the Sedimentary Basins

EGU2008-A-03197;  SM6-1TH5P-0524
Wüstefeld, A; Bokelmann, GHR; Barruol, G
Lithospheric anisotropy beneath the East European Craton

EGU2008-A-09119;  SM6-1TH5P-0525
Artemieva, I M
Dynamic Topography of the East European Craton: mantle downwelling in the interior with mantle upwellings at the margins?

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