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Integral equation method in two dimensions

For such geoelectrical models, the electric field has but a single component, Ey, which can be represented as the sum of a background (normal) part and an anomalous part  [Pg.234]

It should be clear that the total field, Ey, satisfies the equation [Pg.234]

Subtracting the last equation from the one before it, we find an equation for the anomalous field  [Pg.234]

An important role is played in the integral equation method by the Green s function for the background (normal) model of the earth. The Green s function, Gft(r lr), depends on the positions of two points, M(r) and M (r ), and is determined by a solution of the equation  [Pg.235]

In this last equation, 6 is the two dimensional Dirac delta-function which is defined as follows  [Pg.235]


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