La misura della disomogeneità di magnetizzazione delle rocce
Main Article Content
Abstract
The use of the magnetometer, previous described by the
A., in the measure of the magnetization inliomogeneity of a rock sample
is shown in the present paper.
At the first it is studied the signal generated in this magnetometer by
an off-centre dipole; after it is proposed to reduce a rock sample to a sample
uniformly magnetized in a direction with an off-centre dipole no necessary
parallel to that direction.
With this scheme the A. introduces a measure, that it named the index
of the magnetization inliomogeneity : of course this index can do an idea
of the eventual inhomogeneity of the rock sample.
A., in the measure of the magnetization inliomogeneity of a rock sample
is shown in the present paper.
At the first it is studied the signal generated in this magnetometer by
an off-centre dipole; after it is proposed to reduce a rock sample to a sample
uniformly magnetized in a direction with an off-centre dipole no necessary
parallel to that direction.
With this scheme the A. introduces a measure, that it named the index
of the magnetization inliomogeneity : of course this index can do an idea
of the eventual inhomogeneity of the rock sample.
Article Details
How to Cite
CIALDEA, R. (1968) “La misura della disomogeneità di magnetizzazione delle rocce”, Annals of Geophysics, 21(1), pp. 1–14. doi: 10.4401/ag-5056.
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