Shear wave anisotropy of laminated lower crust beneath Urach (SW Germany): a comparison with xenoliths and with exposed lower crustal sections

Author:

Rabbel W,Siegesmund S,Weiss T,Pohl M,Bohlen T

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference68 articles.

1. Long-wave elastic anisotropy produced by horizontal layering;Backus;J. Geophys. Res.,1962

2. Seismic anisotropy and shear-wave splitting in lower-crustal and upper-mantle rocks from the Ivrea Zone—experimental and calculated data

3. 3-D seismic velocities calculated from lattice-preferred orientation and reflectivity of a lower crustal section: examples of the Val Sesia section (Ivrea Zone, northern Italy);Barruol;Geophys. J. Int.,1993

4. Bartelsen, H., Lüschen, E., Krey, Th., Meissner, R., Schmoll, H., Walther, C., 1982. The combined seismic reflection-refraction investigation of the Urach Geothermal Anomaly. In: Händel, R. (Ed.), The Urach Geothermal Project. Schweitzerbart, Stuttgart, pp. 247–262.

5. Direct evidence for the composition of the lower crust and the Moho;Berckhemer;Tectonophysics,1969

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