Metamorphism and structure of the Cambrian-Ordovician sediments in southwest Nelson district
The geology of the Victoria Range and the Maruia Upper Grey depression in Springs Junction district has been examined with particular emphasis on metamorphisms and structures. The 'Z?' sediments in the Victoria Range are correlated with the Aorere Group of NW Nelson on the basis of their...
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| Language: | en |
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University of Canterbury. Geology
2013
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| Online Access: | http://hdl.handle.net/10092/7494 |