The Anatoki fault and structure of the adjacent Buller and Takaka terrane rocks, northwest Nelson, New Zealand
The Early Paleozoic rocks exposed in the northwest of the South Island, New Zealand, can be grouped into two terranes. An Ordovician deep water passive margin assemblage makes up the Buller terrane. A Cambrian arc assemblage and an Ordovician to Silurian mainly shallow water passive margin assemblag...
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| Language: | en |
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University of Canterbury. Geology
2010
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| Online Access: | http://hdl.handle.net/10092/4758 |