Kinematics of the Paparoa Metamorphic Core Complex, West Coast, South Island, New Zealand.
The Paparoa Metamorphic Core Complex developed in the Mid-Cretaceous due to continental extension conditioning the crust for the eventual breakup of the Gondwana Pacific Margin, which separated Australia and New Zealand. It has two detachment systems: the top-NE-displacing Ohika Detachment at the no...
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| Language: | en |
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University of Canterbury. Geological Sciences
2011
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| Online Access: | http://hdl.handle.net/10092/5459 |