1887

Abstract

Application of original method for geological modeling are discussed. Method used isostatic compensation, gravity and bathymetry data for deep geological section. Algorithm calculates layer depths and absolute densities. Method permits to find of perspective mineral deposits. Development used for modelling of the Azores region. Spreading Terceira Rift are explained by mantle diapir.

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/content/papers/10.3997/2214-4609.20130596
2013-06-10
2026-02-11

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