Abstract
We always use Bouguer anomelies for solving task of interpolationvalues Bouguer anomalies into grid of national gravimetric database. Conditionfor that is values Bouguer anomalies are changed regularly and their covarinacevariance matrix is linearly first order polynomial. However in mountainous regions (over 1500 m), fromstatic conpesation effect suddenly, this condition is not satislied. Because inthis case we must use value topographic isostatic anomalies. On this article weshall analyse sense of topographic isostatic anomalies.
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