Magnetometry of enderbites in Gaisin block of Ukrainian shield

Authors

  • M.N. Reshetnyk National Science Geological Museum NASU, Kiev, Ukraine

Keywords:

Development rate, Safflower, Varieties, Planting date, Temperature, Day length

Abstract

The actual problems of detail studying and cartography of Ukrainian PreCambrian Shield were used. The aim of work was to werify possibility of check whether enderbity create high value of the magnetic field and how they can be visualized on the map.  The magnetic susceptibility and thermomagnetic analysis of enderbytes were investigated. It is shown that enderbytes do not produce the great amounts of MagneticField, but they have a highest induction of magnetic field against the background of others  weak-magnetic rose granites.

References

Description of magnitometrics. http://agico.com

Instruction magnitometrics.http://users.monash.edu.au/~rjarmit/Mag_sus_meter_instructions/KappaMeter_KT9/ KT9_manual.pdf

Katyuk, I., et al., 1992. Group Geological Survey 1: 50,000 with the general search area sheets of M-35-119 A, B - 120, B, (Gysin) // Report geol.- shooting squad for 1987 - 1991- Kiev, 345.

LAM-24-instruction https://sites.google.com/a/g.unibuc.ro/paleomag/home/old-paleomagnetic-laboratory.

Lysek, A., et al., 2006. Formational analysis the lower range of the Precambrian of the Ukrainian shield during geological survey // Kiev, 203.

Reshetnyk, M.N., 2012. The complex magnetic scanning as an effective method to investigate the exposures of Precambrian Basement: example of Ukrainian shield // Sci. J. Pur. App. Sci. 1(1), 22–29. http://www.sjournals.com/index.php/SJPAS/article/view/239/pdf

Published

2015-10-28

How to Cite

Reshetnyk, M. . (2015). Magnetometry of enderbites in Gaisin block of Ukrainian shield. Scientific Journal of Review, 4(10), 193-198. Retrieved from http://sjournals.com/index.php/sjr/article/view/99

Issue

Section

Geography