Titlebook: Seismic Anisotropy in the Earth; V. Babuska,M. Cara Book 1991 Springer Science+Business Media Dordrecht 1991 Pet.crystal.earth.grain.miner

PLE

V. Babuska,M. Carae dedicated to the application of the interpola­ tion theory results to several other problems (the extension problem, generalized stationary processes, spectral theory, nonlinear integrable equations, functions with operator arguments). 2. Now we shall proceed to a more detailed description of the

Largess

V. Babuska,M. Carae dedicated to the application of the interpola­ tion theory results to several other problems (the extension problem, generalized stationary processes, spectral theory, nonlinear integrable equations, functions with operator arguments). 2. Now we shall proceed to a more detailed description of the

precede

V. Babuska,M. Carawe introduce the product measure. We show that if the support of the measure μ consists of more than one point (otherwise there is no randomness), then .. almost every Schur function .. is inner. If, in addition, the logarithmic integral converges: ., then for .. almost every Schur function the sequ

宣称

V. Babuska,M. Caraetries. The applications include: general matrix quadratic equations, the continuous and discrete algebraic Riccati equations, minimal factorization of rational matrix functions with symmetries and the transport equation from mathematical physics. 4. Several matrix decompositions: polar decompositio

attenuate

菊花

Anisotropic structures in the lithosphere,general framework, preferred orientation of minerals may occur in different locations and seismic anisotropy may show up at different scales as a consequence of oriented geodynamic processes during the formation of the lithosphere or, probably more locally, during later tectonic episodes.

袋鼠

发源

Basilar-Artery

Elastic anisotropy of rock-forming minerals and polycrystalline rocks, the physical conditions in the Earth’s interior, provide the necessary basis for realistic interpretations of seismological observations. Velocities of elastic waves are measured in single crystals, naturally occurring rocks and in hot-pressed polycrystalline aggregates. The velocities in rocks and

确定

Interpretation of seismic data in terms of anisotropy,dels. Seismologists are used to employing the word “noise” to explain why their models do not fit the data better. Even if part of the misfit is recognised as of deterministic nature, it is often small enough to be considered as due to some second order effects which are not taken into account in th