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  Poster Programme - TS33 Faulting, flow, and the role of fluids in crustal deformation

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Convener: Kurz, W.
Co-Convener: Rutter, E., Brosch, F., Burlini, L., Holdsworth, R., Kühn, M., Lehner, F., Ritter, O., Schilling, F., Sheldon, H., Vauchez, A., Wibberley, C.
Co-Sponsorship:


Author in Attendance:

Thursday, 28 April 2005 17:30 - 19:00
Display Time: Thursday, 28 April 2005 08:00 -
Thursday, 28 April 2005 19:00
Poster Area: Hall Z

Chairperson: N.N.

Select complete timeblock
Z219
EGU05-A-09494;  TS33-1TH5P-0219
Regenauer-Lieb, K.; Yuen, D.A.
Quartz Rheology and Short-Timescale Crustal Instabilities (cancelled)

Z220
EGU05-A-10793;  TS33-1TH5P-0220
Wibberley, C.
Coseismic and inter-seismic strength changes due to frictional heating and diffusion of slip zone pore fluids in a seismogenic fault zone

Z221
EGU05-A-01147;  TS33-1TH5P-0221
Engström, A.; Skelton, A.
Geochemical mapping of fault architecture and permeability structure of a detachment fault system

Z222
EGU05-A-08093;  TS33-1TH5P-0222
Herwegh, M.; de Bresser, J.H.P; ter Heege, J.
Combining natural microstructures with composite flow laws: An improved approach for the extrapolation of lab data to nature?

Z223
EGU05-A-08925;  TS33-1TH5P-0223
Grasemann, B.; Martel, S.; Passchier, C.
The origin of fault drag and its implications for the geometry and mechanics of faults

Z224
EGU05-A-00188;  TS33-1TH5P-0224
Gessner, K.; Kuehn, M.
3D Numerical modelling of strain localization, fluid flow and reactive transport related to hydrothermal mineralisation at Mount Isa, Australia

Z225
EGU05-A-06536;  TS33-1TH5P-0225
Kühn, M.; Gessner, K.
2D or not 2D: Are two Dimensions enough to accurately model Convective Fluid Flow through Faults and surrounding Host Rocks?

Z226
EGU05-A-02348;  TS33-1TH5P-0226
Neubauer, F.; Nemes, F.
Anatomy of a fault zone: the Periadriatic fault

Z227
EGU05-A-03973;  TS33-1TH5P-0227
Gessner, K.; Kuehn, M.; Sheldon, H.; Ord, A.; Schaubs, P.M.; Potma, W.; Hobbs, B.E.; Zhang, Y.; Zhao, C.; Roberts, P.A.
Simulation of deformation, fluid flow, heat transfer, species transport, and chemical reactions in hydrothermal ore systems

Z228
EGU05-A-05078;  TS33-1TH5P-0228
Dresen, G.; Bohnhoff, M.; Backers, T.
Spatial and temporal variations of fault zone stresses

Z229
EGU05-A-08809;  TS33-1TH5P-0229
Winkler, G; Reichl, P
Fracture network analysis of faulted and lower deformed carbonates and quartzites on the example of the investigation area Sonnwendstein/Semmering, Austria

Z230
EGU05-A-06516;  TS33-1TH5P-0230
Kühn, M.; Dobert, F.; Gessner, K.
The Significance of heterogeneous Permeability in Faults and fractured Rock Masses on free Convection for the hydrothermal System at Mount Isa, Australia

Z231
EGU05-A-03897;  TS33-1TH5P-0231
Hürzeler, J.-P.; Abart, R.; Schmid, S.
Feedback between fluid-rock interaction, mineral reaction and deformation at the Glarus Thrust (Switzerland)

Z232
EGU05-A-03666;  TS33-1TH5P-0232
Erzinger, J.; Kümpel, H.-J.; Shapiro, S.; KTB-VB Science, Team
Probing a fault zone on the kilometre scale – Experience from massive pumping and injection tests in the 4 km deep KTB pilot hole, Bavaria

Z233
EGU05-A-02492;  TS33-1TH5P-0233
Takahashi, M; Li, X; Kwasniewski, M; Takemura, T; Kato, M
Permeability evolution in the final fault plane - experimental observatins of sandstone under general stress state -

Z234
EGU05-A-01114;  TS33-1TH5P-0234
Plotnikova, I.
Precambrian crystalline Basement of the Tatarstan and the Origin of Oil Fields

Z235
EGU05-A-08751;  TS33-1TH5P-0235
Alt-Epping, P.; Zhao, C.; Hobbs, B.
3D reactive transport simulations of coupled processes in fault planes: implications of chemically induced permeability evolution for the efficiency of ore formation (cancelled)

Z236
EGU05-A-03167;  TS33-1TH5P-0236
Baietto, A.; Cadoppi, P.; Martinotti, G.; Perello, P.; Vuataz, F.-D.; Perrochet, P.
Mechanisms of up-rise of the hot thermal springs of Valdieri (Argentera Massif, Maritime Alps, northwestern Italy)

Z237
EGU05-A-05637;  TS33-1TH5P-0237
Brenner, S.L.; Gudmundsson, A.
Fluid transport in faults and associated hydrofracture injection into host rocks

Z238
EGU05-A-05125;  TS33-1TH5P-0238
Schubnel, A.; Fortin, J.; Thompson, B.; Young, R. P.
Fracture Propagation, Stable Sliding and Stick Slip by Pore Pressurization in a Fault Gouge Analog

Z239
EGU05-A-10944;  TS33-1TH5P-0239
Raphanel, J. L.; Rakotoniriana, M.; Lehner, F. K.
Accuracy of approximate driving force for intergranular pressure solution (cancelled)

Z240
EGU05-A-00904;  TS33-1TH5P-0240
Clark, C; Schmidt Mumm, A; Faure, K
The role of fluid chemistry in brittle failure and breccia formation during synmetamorphic fluid flow and shear zone formation: an example from the Curnamona Province, Australia.

Z241
EGU05-A-06386;  TS33-1TH5P-0241
Krenn, K.; Hoinkes, G.; Fritz, H.
Exhumation history of the Schneeberg Complex west of the Tauern Window

Z242
EGU05-A-09420;  TS33-1TH5P-0242
Kopf, A.J.; Deyhle, A.; Castillo, P.R.
Fluid-rock interaction at temperatures from diagenesis to seismogenesis: The Nankai accretionary complex (Japan)

Z243
EGU05-A-10560;  TS33-1TH5P-0243
Song, S.R.; Chen, Y.L.; Liu, C.M.; Ku, W.Y.; Chen, H.F.; Liu, Y.J.; Yang, T.F.; Chen, C.H.; Liu, T.K.; Lee, M.
Hydrochemical changes of spring waters in Taiwan: implications for evaluating monitoring sites of earthquake precursory

Z244
EGU05-A-06505;  TS33-1TH5P-0244
Vauchez1, A; Egydio-Silva, M; Uhlein, A; Tommasi, A
Distributed strain in an orogen-scale thrust system affecting an anatectic-magmatic segment of the Ribeira-Araçuai belt, Brazil

Z245
EGU05-A-02309;  TS33-1TH5P-0245
RUTTER, E.; Brodie, K.; Irving, D.
How strong are crustal rocks when they start to melt? An experimental study of the flow of partially-molten synthetic ‘granite‘ under undrained conditions.

Z246
EGU05-A-08302;  TS33-1TH5P-0246
Heilbronner, R.; Tullis, J.
Orientation Tracking - a quantitative description of pole figure development in experimentally deformed and dynamically recrystallizing quartzite

Z247
EGU05-A-02698;  TS33-1TH5P-0247
Rossi, M.; Vidal, O.; Wunder, B.
Experimental study of deformation processes within an aggregate under isotropic conditions

Z248
EGU05-A-04995;  TS33-1TH5P-0248
Pauselli, C.; Federico, C.
Lithospheric behaviour and extensional regime in the Northern Apennines: suggestions from rheological profile

Z249
EGU05-A-05202;  TS33-1TH5P-0249
Jefferies, S.; Holdsworth, R.; Wibberley, C.; Shimamoto, T.; Spiers, C.
Fault rock weakening mechanisms along plate-boundary faults: insights from the Median Tectonic Line, Japan

Z250
EGU05-A-01872;  TS33-1TH5P-0250
Fusseis, F.; Handy, M. R.
Evolution of a weak fault at the fossil brittle-to-viscous transition, Cap de Creus, Spain

Z251
EGU05-A-03157;  TS33-1TH5P-0251
Delle Piane, C.; Burlini, L.
Reaction enhanced large strain deformation: decarbonatation of dolomite in torsion experiments

Z252
EGU05-A-09915;  TS33-1TH5P-0252
Heilbronner, R.; Keulen, N.
Shape analysis of experimental and natural fault rocks

Z253
EGU05-A-05843;  TS33-1TH5P-0253
Louis, L.; Baud, P.; Tembe, S.; Wong, T.-f.
Compactant strain localization in an anisotropic sandstone inferred from x-ray ct imaging

Z254
EGU05-A-04542;  TS33-1TH5P-0254
Janssen, C.; Hoffmann-Rothe, A.; Matar, A.; Khatib, M.; Dresen, G.
Different Styles of Faulting Deformation along the Dead Sea Transform

Z255
EGU05-A-04044;  TS33-1TH5P-0255
Nappi, R.; Scarano, I.; Ferranti, L.; Vilardo, G.
Spatial and temporal evolution of low-energy sequences (1990, 1991-1992 and 1997) in the Sannio area (Southern Apennines, Italy) in relation to the existing structural discontinuities: implication for the seismogenic potential

Z256
EGU05-A-03640;  TS33-1TH5P-0256
Arnberger, K; Grasemann, B; Draganits, E; Habermüller, M; Schmid, N
Rheologically controlled fault-related folds (Hallstatt, Northern Calcareous Alps, Austria)

Z257
EGU05-A-01811;  TS33-1TH5P-0257
Moore, D.
Review of Evidence for a Weak San Andreas Fault




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