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
Magnetic field of three-dimensional sources of arbitrary shape on a non-horizontal plane
1982 V. V. Glazunov
Compilation of three-dimensional structural-plane models of the crust of the eastern part of the Baltic Shield
1982 E. A. Levenberg
Use of exchange refracted waves in the study of the Pechenga area
1982 T. L. Pisakina, T. B. Gavlovskaya