Use of Vertical Gradients for Interpretation of Gravimagnetic Anomalies (Ispolzovanie Vertikalnykh Gradientov dlya Interpretatsii Gravimagnitnykh Anomalii).

摘要

This report elaborates on the methods possible for direct determinations of the vertical gradients and accelerated computations. It also discusses the advantages of vertical gradients; their direct measurement gives the most accurate initial data for interpretation.