On the use of anhysteretic remanent magnetization in paleointensity determination

Details On the use of anhysteretic remanent magnetization in paleointensity determination On the use of anhysteretic remanent magnetization in paleointensity determination

Jan 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977pepi...13..360b&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 13, Issue 4, p. 360-362.

Physics

6

Scientific paper

The relative intensities of anhysteretic remanent magnetization (RAM) and thermoramanent magnetization (TRM) are strongly dependent on grain size, blocking temperature and applied field, and are poorly predicted by existing theories. Analog techniques that substitute ARM for TRM probably yield adequate relative paleointensities in suites of mineralogically similar rocks, but they yield uncertain estimates of absolute paleointensity.

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