The magnetic fabric of the Late Permian Dundee ignimbrite, Dundee, N.S.W

M. A. Lackie

Research output: Contribution to journalArticlepeer-review

Abstract

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.

Original languageEnglish
Pages (from-to)481-488
Number of pages8
JournalExploration Geophysics
Volume19
Issue number4
DOIs
Publication statusPublished - 1988

Keywords

  • Dundee ignimbrite
  • Ignimbrites
  • Late permian
  • Magnetic fabric
  • Magnetic foliation
  • Magnetic lineation

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