
%0 Journal Article
%A Lackie, M.A. 
%T The magnetic fabric of the Late Permian Dundee Ignimbrite, Dundee, N.S.W.
%J Exploration Geophysics
%D 1988/12/01
%V 19
%N 4
%P 481-488
%K 
%R https://doi.org/10.1071/EG988481
%U https://www.publish.csiro.au/paper/EG988481 
%X The Dundee Ignimbrite has a distinct magnetic fabric, defined by susceptibility anisotropy. Magnetic foliation data for the ignimbrite mass at Dundee define a basinal structure. The magnetic lineation data which are argued to be flow lineations generally have a NNE?SSW orientation. This suggests that the source vent(s) for the ignimbrite is external to the mass. 
