Comparative measurements of magnetic susceptibility anisotropy in red sandstones

Details Comparative measurements of magnetic susceptibility anisotropy in red sandstones Comparative measurements of magnetic susceptibility anisotropy in red sandstones

Aug 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988pepi...51..320h&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 51, Issue 4, p. 320-325.

Physics

1

Scientific paper

The anisotropy of magnetic susceptibility of Triassic red sandstones from northern Bavaria (Plattensandstein Formation) is very weak within the maximum susceptibility plane. The anisotropy resulting from the shape and size of cylindrical red bed samples can exceed and obscure the lineation of the sedimentary fabric when measured with a spinner magnetometer. This frequently observed error can be eliminated when the cylindrical specimens are drilled perpendicular to bedding. Alternatively, cubic samples which are measured on a susceptibility bridge, are not affected by this error.

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