EGU General Assembly 2008
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  List of Accepted Contributions - TS13 Structure and dynamics of orogenic wedges

Please, click Abstract Number to find the corresponding abstract as PDF file; if necessary, download Adobe Acrobat Reader 4.0 first to open the file. Authors of "no-abstract" papers are invited to upload their abstracts, and authors of DOC-File, Email or Hard-Copy submissions are invited to proof-read their abstracts edited by the secretariat (see "Abstract Information" on the conference home site). Any abstract may be freely reproduced for non-commercial, scientific purposes; however, the moral right of the author(s) to be identified as the author(s) of such abstracts is asserted.

EGU2008-A-00972
Husson, L.; Brun, J-P.; Faccenna, C.; Gueydan, F.; Royden, L. H.
Transient subduction rollback as a mechanism for blueschists exhumation

EGU2008-A-01937
Booth-Rea, G.; Klaeschen, D.; Grevemeyer, I.; Reston, T.
Heterogeneous deformation in the Cascadia convergent margin and its relation to thermal gradient (Washington, NW EEUU)

EGU2008-A-02046
Callot, JP; Monticone, B; Pillot, D
Analogue models of multi-layer brittle ductile wedges, and comparison with natural examples

EGU2008-A-02236
Engl, D.A.; Ortner, H.
Large-scale fold structures in the Tauern Window involving both Penninic and Austroalpine units?

EGU2008-A-02358
Stanica, D.; Stanica, D.A.
An improved geodynamic model for the seismic active Vrancea zone, Romania

EGU2008-A-03319
Precigout, J.; Gueydan, F.; Gapais, D.
Mantle ductile deformation beneath a continental rift: insight from the structural study of the Ronda massif (southern Spain)

EGU2008-A-03890
Messager, G.; Nivière, B.; Lacan, P.; Martinod, J.; Xavier, J.P.
Interplay between thick- and thin-skinned tectonics along fold and thrust belts. Example of the Andean foothill (Neuquén basin, Argentina)

EGU2008-A-03964
Philippon, M.; Brun, J-P; Gueydan, F
Deciphering subduction from exhumation in the blueschists of the Ile de Groix (Hercynian belt of Brittany, W France)

EGU2008-A-04199
Hoth, S.; Thiede, R. C.; Kukowski, N.; Oncken, O.; Avouac, J-P.
Internal versus external forcing of orogenic detachments

EGU2008-A-04262
Booth-Rea, G.; Martínez-Martínez, J.M.; Azañón, J.M.
Thermal consequences of syn-orogenic extension: example of the Sierra Nevada elongated dome (Western Mediterranean)

EGU2008-A-04788
Belova, A. A.; Kuznetsov, N. B.; Ryazantsev, A. V.
The Vendian - Early Paleozoic tectonic evolution of the Southern Urals

EGU2008-A-04297
Zámolyi, A.; Decker, K.; Hölzel, M.; Strauss, P.; Wagreich, M.
Kinematics and timing of deformation at the front of the Alpine-Carpathian wedge

EGU2008-A-06487
Bausa, J.; Tavani, S.; Muñoz, J.A.; Storti, F.
3D fracture pattern in the Fiastrone anticline, Sibillini thrust sheet, Northern Apennines (Italy)

EGU2008-A-07115
Brun , JP; Faccenna, C
Exhumation of high-pressure rocks driven by slab rollback in the Aegean

EGU2008-A-07390
Carry, N.; Brun, J.P.; Vrielynck, B.; Gueydan, F.; Marquer, D.
Exhumation of HP-UHP units in the Alps: the role of subduction rollback.

EGU2008-A-07406
Martínez-Martínez, J.M.; Booth-Rea, G.
Miocene upper-crustal extension and coeval mid-crustal shortening in the hinterland of the Betics (western Mediterranean)

EGU2008-A-07895
Souloumiac, P.; Cubas, N.; Leroy, Y. M.; Maillot, B.
Predicting in-situ stress and thrusting sequences in accretionary wedges

EGU2008-A-09392
Gueydan, F; Booth-Rea, G; Martinez-Martinez, J M ; Garrido, C
Continental subduction and back-arc extension in the western Mediterranean. Insights from simple 1D PT path numerical models

EGU2008-A-09424
Gueydan, F; Le Garzic, E; Carry, N
Geometry and kinematics of continental subduction inferred from 1D thermal modelling of prograde PT path

EGU2008-A-09694
Ortner, H.; Thöny, W.; Reiter, F.
Forward and hindward propagation of thrusting from Miocene – Recent in the Alps of Western Austria

EGU2008-A-12249
Warren, C J ; Beaumont, C; Jamieson, R A ; Lee, B
Formation, detachment and exhumation of ultra-high-pressure rocks during continental subduction: Implications for ‘extension’ in convergent orogens


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