Geological Interpretation of Poladauri Magnetic Anomaly

Author: Guram Kutelia
Co-authors: n. abutidze, n. Lursmanashvili, n. Tsulaia
Keywords: Poladauri Magnetic Anomaly, Poladauri Deposite
Annotation:

Geological Interpretation of Poladauri Magnetic Anomaly From a number of ore occurrence identified on the territory of Georgia one of the significant iron Deposit is on the territory of Poladauri of the Bolnisi district. In the sixties of the last century, the carried-out magnetic survey of this territory showed the insolvency of a magnetic exploration for detection of deposits, as a mineral hematite, which contains 70% of iron, due to its antiferromagnetism creates a magnetic field of low power. Surveys which are carried out by modern equipment gave the possibility to determine the depth and form of a bedding of the bodies causing the magnetic anomalies, which well coordinated with the data which are received from wells drilled on this area.

Lecture files:

ფოლადაურის მაგნიტური ანომალიის გეოლოგიური ინტერპრეტაცია [ka]