Titlebook: Mathematics for Seismic Data Processing and Interpretation; A. R. Camina,G. J. Janacek Book 1984 A. R. Camina and G. J. Janacek 1984 geoph

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Applications,To conclude our review of the mathematics behind signal processing we shall look at some rather specific applications. We will discuss.As you might expect our survey will not be comprehensive but we expect that our readers will be able to read the original articles with some understanding.

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A. R. Camina,G. J. Janaceklar medium, they interact with a large-scale magnetic ?eld such as the magnetic ?eld of the Sun or the Galactic magnetic ?eld. As these background ?elds are usually nearly constant in time and space, they can be approximated by a homogeneous ?eld. If there are no additional ?elds, the particle traje

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A. R. Camina,G. J. Janacekof the Sun or the Galactic magnetic ?eld. As these background ?elds are usually nearly constant in time and space, they can be approximated by a homogeneous ?eld. If there are no additional ?elds, the particle trajectory is a perfect helix along which the par- cle moves at a constant speed. In reali

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A. R. Camina,G. J. Janaceklar medium, they interact with a large-scale magnetic ?eld such as the magnetic ?eld of the Sun or the Galactic magnetic ?eld. As these background ?elds are usually nearly constant in time and space, they can be approximated by a homogeneous ?eld. If there are no additional ?elds, the particle traje

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A. R. Camina,G. J. Janacekof the Sun or the Galactic magnetic ?eld. As these background ?elds are usually nearly constant in time and space, they can be approximated by a homogeneous ?eld. If there are no additional ?elds, the particle trajectory is a perfect helix along which the par- cle moves at a constant speed. In reali

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