Cenozoic distributed rotational deformation, South Island, New Zealand
New structural and paleomagnetic data from the Marlborough region, New Zealand, provide better constraints on the timing of the formation of the South Island orocline. These data indicate that approximately 100° of clockwise bending of the crust has occurred across this part of the plate boundary zo...
| Main Authors: | , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2004
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