Remagnetisation of strata during the hunter-bowen orogeny

M. A. Lackie; P. W. Schmidt

doi:10.1071/EG993269

Remagnetisation of strata during the hunter-bowen orogeny

M. A. Lackie, P. W. Schmidt

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

19 Citations (Scopus)

Abstract

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 language	English
Pages (from-to)	269-274
Number of pages	6
Journal	Exploration Geophysics
Volume	24
Issue number	2
DOIs	https://doi.org/10.1071/EG993269
Publication status	Published - 1993
Externally published	Yes

Keywords

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

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10.1071/EG993269

Cite this

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abstract = "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.",

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AU - Schmidt, P. W.

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AB - 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.

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KW - Remagnetisation

KW - Werrie Basalt

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Remagnetisation of strata during the hunter-bowen orogeny

Abstract

Keywords

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