Mapping of the Lower and Upper Cretaceous boundary in the mountainous Crimea by ground magnetic imaging
Abstract
Detailed geologic mapping of sedimentary rock strata based on ground magnetic survey data and solution of structural problems in the areas of their development is sharply limited until now. This is explained by the usually very low magnetization of sedimentary formations, their weak differentiation by magnetic properties and gentle bedding, which is characteristic of the territory under consideration. ...
Область исследования:
(Archived) Without section
Funding:
None
References
- Geology of the USSR, vol. VIII, Crimea, pt. І. Geologic description. M., Nedra, 1969.
- Logachev A.A., Zakharov V.P. Magnetic prospecting. L., Nedra, 1973.
- Popov A.A., Lomakin A.B. Borehole Magnetic Prospecting. In the book: "Borehole Ore Geophysics". L., Nedra, 1971.
Similar articles
Determination of the position of reflecting boundaries in the near-well space using vertical seismic profiling data
1976 Yu. G. Shopin, E. R. Litvinenko
Determination of the nature of seismic waves using combined systems of surface and borehole observations
1976 M. D. Lizinsky
Methodology of fitting geological and structural models according to a given gravity field with the help of enlarged polyhedral elements
1976 G. G. Kravtsov, V. I. Segalovich
Use of electrical exploration in geologic mapping in the mountainous Crimea conditions
1976 E. F. Dorofeeva, S. K. Zaburdin