THERMOMAGNETIC ANALYSIS OF THE PALEOCENE AND EOCENE SEDIMENTS OF THE TALISH MOUNTAINOUS ZONE.

For investigation of the precise paleomagnetic observation firstly magneto-mineralogical observations, in other words investigation of the ferromagnet minerals in the rock should be made. In the article thermomagnetic analysis of the Paleocene and Eocene sediments of the Talish mountainous zone was made. For the thermomagnetic analysis magnetic parameters of the Jrs-magnets are used. Magnetic and mineralogical structure of natural residual magnetization carriers is observed by the forms of the curve and the blocking of the temperature T. The results of the determination of magnetic curvature of J observations made in Talish zone shows that main carriers of the residual magnetization are magnetite and hematite. [ABSTRACT FROM AUTHOR]