Structure and metamorphism of the Haast Schist and Torlesse Zones between the Alpine Fault and the D'urville Valley, South Nelson
Within the bends region of the Alpine Fault two structural trends have been identified. These are a D1-D2 “Rangitata” trend and a D3 “Kaikoura” trend. The D1 - D2 trend maintains a northeasterly strike of both bedding and S2 schistosity which is independent of the Alpine Fault, intersecting in such...
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| Language: | en |
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University of Canterbury. Geology
2012
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| Online Access: | http://hdl.handle.net/10092/6703 |