Experimental and texture-derived P-wave anisotropy of principal rocks from the TRANSALP traverse: An aid for the interpretation of seismic field data

Author:

Ullemeyer Klaus,Siegesmund Siegfried,Rasolofosaon Patrick N.J.,Behrmann Jan H.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference52 articles.

1. The elastic properties of rock forming minerals;Aleksandrov;Izv. Acad. Sci. USSR, Geophys. Ser.,1961

2. Elastic wave velocities in minerals at atmospheric pressure and increasing precision of elastic constants by means of EVM;Aleksandrov;Izv. Acad. Sci. USSR, Geol. Ser.,1974

3. Experimental and theoretical tools for characterizing anisotropy due to mechanical defects in rocks under varying pore and confining pressures;Arts,1996

4. 3D seismic study of a ductile shear zone from laboratory and petrofabric data (Saint Barthélémy Massif, Northern Pyrénées, France);Barruol;Terra Nova,1992

5. Zur Kinematik der Kontinentkollision in den Ostalpen;Behrmann;Geotekton. Forsch,1990

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