Titlebook: Introduction to Complex Theory of Differential Equations; Anton Savin,Boris Sternin Textbook 2017 Springer International Publishing AG 201

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Anton Savin,Boris Sterninptic curves in computing theory and coding theory. In the third appendix we discuss the role of elliptic curves in homotopy theory. In these three introductions the reader can get a clue to the far-reaching implications of the theory of elliptic curves in mathematical sciences. During the ?nal produ

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Anton Savin,Boris Sterninse of elliptic curves in computing theory and coding theory. In the third appendix we discuss the role of elliptic curves in homotopy theory. In these three introductions the reader can get a clue to the far-reaching implications of the theory of elliptic curves in mathematical sciences. During the

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Anton Savin,Boris Sterninse of elliptic curves in computing theory and coding theory. In the third appendix we discuss the role of elliptic curves in homotopy theory. In these three introductions the reader can get a clue to the far-reaching implications of the theory of elliptic curves in mathematical sciences. During the

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ptic curves in computing theory and coding theory. In the third appendix we discuss the role of elliptic curves in homotopy theory. In these three introductions the reader can get a clue to the far-reaching implications of the theory of elliptic curves in mathematical sciences. During the ?nal produ

Complement

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Asymptotics of ramified integrals, description of these singularities. The aim of this chapter is to answer this question. In more detail, we study ramified integrals near generic points of Landau manifolds. Namely, we show that the ramification of the homology class, over which we integrate, is described by Picard–Lefschetz formula

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Balayage inwards problem,ely, the problem of sweeping the charge is reduced to a problem for a differential equation in a real domain and we will show how one can (and should!) study the latter problem using methods of complex theory.

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Mother body problem,ng the form and mass density of this body. Similar problems appear in geoprospecting, where one measures the gravitational field on the ground surface and wants to determine the source of this gravitational field located inside the earth. Clearly, the solution of this problem is not unique. For exam