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

M. A. Lackie

doi:10.1071/EG988481

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

M. A. Lackie

Faculty of Science and Engineering

Research output: Contribution to journal › Article › peer-review

1 Citation (Scopus)

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 language	English
Pages (from-to)	481-488
Number of pages	8
Journal	Exploration Geophysics
Volume	19
Issue number	4
DOIs	https://doi.org/10.1071/EG988481
Publication status	Published - 1988

Keywords

Dundee ignimbrite
Ignimbrites
Late permian
Magnetic fabric
Magnetic foliation
Magnetic lineation

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10.1071/EG988481

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KW - Magnetic lineation

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

Abstract

Keywords

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