Joint interpretation of upper-mantle anisotropy based on teleseismic P-travel time delays and inversion of shear-wave splitting parameters
- 30 June 1996
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 95 (3-4) , 293-309
- https://doi.org/10.1016/0031-9201(95)03122-7
Abstract
No abstract availableThis publication has 38 references indexed in Scilit:
- Small-scale sublithospheric continental mantle deformation: constraints fromSKSsplitting observationsGeophysical Journal International, 1995
- Regional fabric of the deep lithosphere in central Europe from seismic anisotropyStudia Geophysica et Geodaetica, 1995
- Lithospheric thickness and velocity anisotropy—seismological and geothermal aspectsTectonophysics, 1993
- Models of seismic anisotropy in the deep continental lithospherePhysics of the Earth and Planetary Interiors, 1993
- The lithosphere in central Europe—seismological and petrological aspectsTectonophysics, 1992
- The deep lithosphere in the Alps: a model inferred from P residualsTectonophysics, 1990
- Seismologically determined deep lithosphere structure in FennoscandiaGeologiska Föreningen i Stockholm Förhandlingar, 1988
- The magnitude, symmetry and origin of upper mantle anisotropy based on fabric analyses of ultramafic tectonitesGeophysical Journal International, 1984
- Travel times and station corrections for P waves at teleseismic distancesJournal of Geophysical Research, 1983
- The lithosphere-asthenosphere system in FennoscandiaTectonophysics, 1982