Structural development of the Dun Mountain Ophiolite Belt in the Permian, Bryneira range, Western Otago, New Zealand.
The deformed Permian Dun Mountain Ophiolite Belt (DMOB) forms the basement of the Dun Mountain-Maitai terrane and is traceable through the entire length of New Zealand. The DMOB contains a variably serpentinised mantle portion and a crustal portion containing gabbros, dolerites, cross cutting dikes...
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| Language: | en |
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University of Canterbury. Geological Sciences
2008
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| Online Access: | http://hdl.handle.net/10092/1587 |