About taking into account the averaging interval when interpreting the difference magnetic anomalies of low thickness strata and simple anticlinal folds.
Authors:
Abstract
To increase the reliability of geological interpretation of aeromagnetic survey materials, often with the help of various transformations try to isolate from the anomalous field component associated mainly with a certain depth interval of magnetic rocks ...
Область исследования:
(Archived) Without section
Funding:
None
Similar articles
Calculation of the seismic model of the lower part of the Earth's crust and the crust-mantle transition zone from GSZ data on the Priladozhsky profile
1982 A. G. Goncharov
Theory and practice of amplitude-phase measurements of harmonic magnetic field interference for the purpose of electrical prospecting
1982 V. Kh. Zakharov
Algorithms of automated processing in solving the problem of classification of bottom sediments by acoustic methods
1982 A. I. Svechnikov