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 | |
| 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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