2-d euler de-convolution through dst of gravity data

نویسندگان

وحید ابراهیم زاده اردستانی

چکیده

the different similarity transformation (dst) technique (stavrev, 1997) utilizes a powerful and fully automatic tool for depth estimation of a point source through euler de-convolution. stavrev (1997) showed the results for the magnetic data of simple 2-d sources and aeromagnetic data along profiles. we apply the technique for the gravity data of 2-d rectangular models and real gravity data which has not been considered by stavrev (1997).

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