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
Compilation of three-dimensional structural-plane models of the crust of the eastern part of the Baltic Shield
1982 E. A. Levenberg
Seismic studies by the transmission method on the Vuori-Järvi massif of alkaline-ultrabasic rocks
1982 M. D. Lizinsky
Magnetic field of three-dimensional sources of arbitrary shape on a non-horizontal plane
1982 V. V. Glazunov