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  Poster Programme - TS3.2 Rupture and creep in the lower continental crust: Evidence from geophysical, geological and petrological observations

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Convener: Meissner, R.
Co-Convener: Jones, A., Kern, H.

Author in Attendance:

Friday, 7 April 2006 13:30 - 15:00
Display Time: Friday, 7 April 2006 08:00 -
Friday, 7 April 2006 19:30
Poster Area: Halls X/Y

Chairperson: MEISSNER, R.

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EGU06-A-02185;  TS3.2-1FR3P-0960
Chiozzi, P.; Pasquale, V.; Verdoya, M.
Seismicity and rheological modelling in an extensional-compressional tectonic realm

EGU06-A-02190;  TS3.2-1FR3P-0961
Pasquale, V.
Effects of crustal heat source redistribution on the strength envelopes

EGU06-A-04381;  TS3.2-1FR3P-0962
Zappone, A.; Burlini , L.; Connolly , J.; Husen , S.; Kissling , E.
Lower crustal seismic velocities and seismicity in the northern Alpine foreland: I. Observations and petrophysical experiments.

EGU06-A-08420;  TS3.2-1FR3P-0963
Strehlau, J.; Stange, St.
Earthquakes in the lower crust under the Northern Alpine Foreland Basin: Seismological detection of active metamorphism?

EGU06-A-07915;  TS3.2-1FR3P-0964
Aldersons, F.; Ben Avraham, Z.; Kissling, E.
Lower-crustal seismicity in the Dead Sea region

EGU06-A-04486;  TS3.2-1FR3P-0965
Rybacki, E.; Dresen, G.
High-temperature ductile failure of feldspar rocks

EGU06-A-05183;  TS3.2-1FR3P-0966
Austrheim, H.
Are the mineralogy and rheology of the lower continental crust and upper mantle fluid controlled?

EGU06-A-09729;  TS3.2-1FR3P-0967
Kummerow, J.; Schilling, F.R.
The influence of intergranular, supercritical water on the elastic properties of amphibolite

EGU06-A-10010;  TS3.2-1FR3P-0968
Bischoff, M. ; Endrun, B.; Meier, T.
Lower crustal anisotropy in Central Europe deduced from dispersion analysis of Love and Rayleigh waves

EGU06-A-06805;  TS3.2-1FR3P-0969
Thompson, A. B.; Lexa, O.; Schulmann, K.; Henk, A.; Schwartz, M.
Role of felsic vs. mafic lower crust in the rheological behaviour of crustal driven orogens (cancelled)

EGU06-A-05890;  TS3.2-1FR3P-0970
Nüchter, J.-A.; Stöckhert, B.
Fracturing and transformation into veins beneath the crustal scale brittle ductile transition – a record of co-seismic loading and post-seismic relaxation

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