Analytical method of interpreting magnetic anomalies of a horizontal plate at inclined magnetization
Authors:
Abstract
Anomalies characteristic of the horizontal plate are most often observed in platform regions. Their sources are usually relatively low thicknesses of terrigenous (sometimes volcanogenic) rocks, the distribution of which in the plan is limited by discontinuities or zones of sharp facies transitions ...
Область исследования:
(Archived) Without section
Funding:
None
Similar articles
Crustal depth section of central Karelia and its seismic model
1981 I. V. Litvinenko, S. A. Ankudinov, I. A. Gavrilov, L. M. Dvoretskaya, K. A. Kalnin, N. N. Matveeva, L. N. Platonenkova, N. G. Romanenko
Kinematic peculiarities and exploration possibilities of exchange waves refracted on steeply dipping contacts
1981 T. B. Gavlovskaya, M. D. Lizinsky
Comparison of seismic data on the upper crust of Iceland and the Baltic Shield
1981 S. M. Zverev, I. V. Litvinenko