Geomagnetic Field of the Black Sea Basin,

Abstract

Observations were made with a sea proton magnetometer along meridional profiles; the average distance between profiles was about 28 km. On some profiles special echo sounders were employed for highly precise depth measurements. Horizontal control of the profiles was with a RSVT-1 radiogeodetic system, as well as by navigation and astronomical methods. Survey data were used in compiling a map of given magnetic field anomalies for a large part of the Black Sea. Five large zones were defined which differ in amplitude, periods and strike of anomalies. Quantitative computations of the parameters of magnetically disturbing bodies were made for determining the geologic nature of 14 anomalies. Comparison of these data with deep seismic sounding data indicates an adequate reliability of determining depth to the upper surface of disturbing bodies. (Author)

Document Details

Document Type
Technical Report
Publication Date
Jul 26, 1971
Accession Number
AD0730077

Entities

People

  • B. D. Uglov
  • G. V. Osipov
  • Ya. P. Malovitskii

Organizations

  • National Air and Space Intelligence Center

Tags

DTIC Thesaurus Topics

  • Amplitude
  • Black Sea
  • Computations
  • Magnetic Fields
  • Magnetometers
  • Measurement
  • Measuring Instruments
  • Navigation
  • Observation
  • Position Finding
  • Reliability
  • Scalar Magnetometers
  • Sonar

Readers

  • Geodesy
  • Oceanography.
  • Space Exploration and Orbital Mechanics.