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List of Accepted Contributions - MPRG16 The role of fluids in faults and fracture zones - transport aspects
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EGU2007-A-00927
Brantut, N.; Schubnel, A.; Brunet, F.; Leroy, Y.; Shimamoto, T.
High velocity frictional properties of pure kaolinite and natural kaolinite-bearing fault gouges |
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EGU2007-A-01457
Dong, J.J.; Hsu, J.Y.; Shimamoto, T.; Hung, J.H.; Yeh, E.C.; Wu, Y.H.
Effective confining pressure dependency for fluid flow properties of young sedimentary rocks from TCDP Hole-A |
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EGU2007-A-01540
Schubnel, A.; Thompson, B.D.; Fortin, J. ; Guéguen, Y. ; Young, R.P.
Fluid-induced rupture of a fault gouge analogue in the laboratory |
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EGU2007-A-01585
David, C.; Louis, L.; Mengus, J.M.
Influence of heterogeneity, anisotropy and induced damage on fluid flow in Bentheim sandstone |
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EGU2007-A-02025
Rath, V. ; Klitzsch, N.
Joint modeling and Bayesian inversion of SP, temperatures and hydraulic data
for geothermal systems |
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EGU2007-A-05360
Doan, M.-L.; Brodsky, E.E.; Agnew, D.C.
Permeability enhancement by seismic waves : the importance of local heterogeneities |
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EGU2007-A-05500
Telenga, K.; Stöckhert, B.
Alteration halos along tensile cracks in natural rocks - fluid infiltration into the permeable damage zone |
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EGU2007-A-06869
Miller, S.A.
Triggering of Landers aftershocks from Hector Mine earthquake due to Overpressured Fluids |
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EGU2007-A-07688
Wibberley, C
Fault zone permeabilities over geological timescales: constraints from sedimentary basins |
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EGU2007-A-07841
Pacchiani, F.; Lyon-Caen, H.
Earthquake migration within a normal fault and implications on rock permeability |
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EGU2007-A-08294
Faulkner, D.; Mitchell, T.; Healy, D.; Heap, M.
Slip on 'weak' faults by the rotation of regional stress in the fracture damage zone |
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EGU2007-A-08584
Gland, N.; Dautriat, J.; Dimanov, A.
Stress dependant permeabilities of sandstones: anisotropic response and end effects |
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EGU2007-A-10336
Moerz, T.; Kreiter, S.; Karlik, E. A.; Kopf, A.
Experimental initiation of fluid venting structures in unconsolidated granular and cohesive sediments |
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