Remagnetisation of strata during the hunter-bowen orogeny

M. A. Lackie, P. W. Schmidt

Research output: Contribution to journalArticlepeer-review

19 Citations (Scopus)


Palaeomagnetic studies of strata within the southern New England Fold Belt show evidence of a northward migration of remagnetisation of the Belt during the Permian. In some rock units, such as the Kiah Limestone a syn-deformational remagnetisation is observed, while in others a pre-folding magnetisation is observed.

Original languageEnglish
Pages (from-to)269-274
Number of pages6
JournalExploration Geophysics
Issue number2
Publication statusPublished - 1993
Externally publishedYes


  • Hunter-Bowen Orogeny
  • Kiah Limestone
  • New England Fold Belt
  • Permian
  • Remagnetisation
  • Werrie Basalt


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