Abstract
The A. describes a new magnetometer realized in the
"Istituto Nazionale di Geofìlica", particularly appointed to determine the
direction of the magnetization intensity, eventually present in the igneous
rocks. In the present paper the A. elaborates the theory of this apparatus
and describes its technical characteristics and its sensibility; at last the
A. proposes the technical method in order to determine the direction of
the magnetization intensity.
"Istituto Nazionale di Geofìlica", particularly appointed to determine the
direction of the magnetization intensity, eventually present in the igneous
rocks. In the present paper the A. elaborates the theory of this apparatus
and describes its technical characteristics and its sensibility; at last the
A. proposes the technical method in order to determine the direction of
the magnetization intensity.
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DOI: https://doi.org/10.4401/ag-5053
Published by INGV, Istituto Nazionale di Geofisica e Vulcanologia - ISSN: 2037-416X