つくばリポジトリ RSI 88 3

В данной работе приводится алгоритм решения обратной динамической задачи сейсмики в частотной области для горизонтально-слоистой среды

We present sufficient conditions for the existence of solutions to Neu- mann and periodic boundary-value problems for some class of quasilinear ordinary differential equations.. We

The object of this paper is the uniqueness for a d -dimensional Fokker-Planck type equation with inhomogeneous (possibly degenerated) measurable not necessarily bounded

In order to study the rheological characteristics of magnetorheological fluids, a novel approach based on the two-component Lattice Boltzmann method with double meshes was proposed,

The time-frequency integrals and the two-dimensional stationary phase method are applied to study the electromagnetic waves radiated by moving modulated sources in dispersive media..

While conducting an experiment regarding fetal move- ments as a result of Pulsed Wave Doppler (PWD) ultrasound, [8] we encountered the severe artifacts in the acquired image2.

Wro ´nski’s construction replaced by phase semantic completion. ASubL3, Crakow 06/11/06

Actually it can be seen that all the characterizations of A ≤ ∗ B listed in Theorem 2.1 have singular value analogies in the general case..