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  Oral Programme - TS9 Paleostress fields from structural kinematics - real or imagined

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Convener: Lisle, R.
Co-Convener: Salvini, F., Simón-Gómez, J.
Co-Sponsorship:

Wednesday, 27 April 2005

Lecture Room: Lecture Room 3

Chairperson: N.N.

Select complete timeblock
8:30 - 8:45
EGU05-A-01407;  TS9-1WE1O-001
Angelier, J.
Do stress-paleostress and deformation analyses provide similar or complementary information in brittle tectonics ?

8:45 - 9:00
EGU05-A-03759;  TS9-1WE1O-002
Kaven, J.O.; Maerten, L.; Pollard, D.D.
Using striation data to understand the mechanics of faulting in heterogeneous stress fields (solicited)

9:00 - 9:15
EGU05-A-04272;  TS9-1WE1O-003
De Vicente, G.; Muñoz Martín, A.; Vegas, R.; Cloetingh, S.; Casas, A.; González-Casado, J.M.; Alvarez, J.
Neutral points and constrictive deformation in paleostresses analysis: The Cenozoic contraction of Iberia.

9:15 - 9:30
EGU05-A-06527;  TS9-1WE1O-004
Liesa, C.L.; Simón, J.L.
Space and time stress partitioning within an intraplate region: Tertiary compressive stress fields in eastern Iberia

9:30 - 9:45
EGU05-A-07824;  TS9-1WE1O-005
Fodor, L.
Stress field variations around overlapping oblique-slip faults with multiple slip events: a case study from the Pannonian rift system

9:45 - 10:00
EGU05-A-09455;  TS9-1WE1O-006
Salvini, F.; Storti, F.
Kinematically- versus dynamically-induced brittle deformations: the Chinese box ambiguity and solution. Application to the Antarctica Cenozoic Tectonics

10:00
END OF SESSION




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