Palaeomagnetic study of some charnockites of the Palni Hills

Details Palaeomagnetic study of some charnockites of the Palni Hills Palaeomagnetic study of some charnockites of the Palni Hills

Jun 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982pepi...28..269r&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 28, Issue 3, p. 269-272.

Physics

Scientific paper

The intensity of natural remanence magnetisation (NRM) is measured along the three mutually-perpendicular directions using an astatic magnetometer. The intensity of induced magnetisation is measured using an apparatus fabricated in the laboratory. The Koenigsberger ratio has been calculated for all the samples and the ratio has been used to test the stability of NRM in the samples. The mean direction of magnetisation is determined from the three components of the NRM intensity. The palaeomagnetic pole position of the samples is determined using the direction of magnetisation and the site location. An attempt has been made to fix the geological age of the charnockites using palaeomagnetic methods.

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