PLE 发表于 2025-3-23 13:10:56
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 theLargess 发表于 2025-3-23 17:25:07
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 theprecede 发表于 2025-3-23 18:03:50
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 发表于 2025-3-23 23:58:56
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 decompositioattenuate 发表于 2025-3-24 04:31:22
http://reply.papertrans.cn/87/8639/863856/863856_15.png菊花 发表于 2025-3-24 08:45:09
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 发表于 2025-3-24 11:30:54
http://reply.papertrans.cn/87/8639/863856/863856_17.png发源 发表于 2025-3-24 15:23:59
http://reply.papertrans.cn/87/8639/863856/863856_18.pngBasilar-Artery 发表于 2025-3-24 22:10:54
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 发表于 2025-3-25 00:48:02
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