
%0 Journal Article
%A Webster, S.S. 
%A Scheibner, E. 
%T Introduction to the magnetic properties of New England granitoids
%J Exploration Geophysics
%D 1984/06/01
%V 15
%N 2
%P 67-73
%K 
%R https://doi.org/10.1071/EG984067
%U https://www.publish.csiro.au/paper/EG984067 
%X The I-type and S-type granitoids of New England, NSW, generally equate to the magnetite-series and ilmenite-series classification. The only non-conforming suite is the Uralla I-type suite which is non-magnetic, but these granitoids also exhibit several abnormal geochemical parameters. The Triassic leuco-adamellites are also non-magnetic, but exhibit magnetic aureoles. Limited remanence measurements are available. Samples of two late-Triassic plutons show strong remanence, indicating allowance will have to be made for such effects in quantitative analysis of magnetic data. 
