par IL. BUCUR
The anhysteretic remanent magnetization (A.R.M.) in steady fields 
of
0,5 and 2 Oe and in alternating fields 
varying
between 25 and 900 Oe has been studied for 5 samples of rocks of different
nature. The study concerned
the A.R.M. obtained by the action of the two fields and
at
various relative orientations: 
,
at
different angles to .
A method for reorienting bore cores using the properties of the A.R.M. is proposed.