The structure of the Buller terrane west of the Anatoki thrust, upper Cobb Valley, Northwest Nelson, New Zealand.
The Buller terrane west of the Anatoki Thrust in the upper Cobb Valley area is composed of Ordovician marine sediments. Rocks in the field area are divided into two domains of different structural styles. In the west Domain 1 includes the Roaring Lion Formation which displays a series of mesoscopic...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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University of Canterbury. Department of Geology
1993
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| Online Access: | https://dx.doi.org/10.26021/8075 https://ir.canterbury.ac.nz/handle/10092/3919 |