Identification of multicomponent anisotropies in rocks using various field and temperature values in a cryogenic magnetometer

Details Identification of multicomponent anisotropies in rocks using various field and temperature values in a cryogenic magnetometer Identification of multicomponent anisotropies in rocks using various field and temperature values in a cryogenic magnetometer

Aug 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988pepi...51..379r&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 51, Issue 4, p. 379-386.

Physics

28

Scientific paper

A new technique involving magnetization measurements on a rotating sample in a cryogenic magnetometer with variable field, from 0 to 4 T, and variable temperature is presented. It can be used to separate and identify multi-component anisotropy in rocks. The results obtained for anisotropy due to magnetite, haematite, pyrrhotite or phyllosilicates are interpreted according to different magnetization models.

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