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
Similar articles
Tracing of steeply dipping reflecting boundaries in plateau basalts of northern Iceland
1982 Wijeratne Makevita
Calculation of theoretical anomalies ∆T at approximation of weakly magnetic geological objects by oblique prisms and polyhedra of general form
1982 G. G. Kravtsov
Compilation of three-dimensional structural-plane models of the crust of the eastern part of the Baltic Shield
1982 E. A. Levenberg