A structural study of the Separation Point Batholith : emplacement mechanisms and the tectonic regime
The Separation Point Batholith is a late Cretaceous granitic intrusion outcropping in the north-west Nelson region of New Zealand. The batholith is elongate, oriented north / south, and stitches the Paleozoic Takaka Terrane to the arc-derived Median Tectonic Zone. It has been found to be related geo...
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| Language: | en |
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University of Canterbury. Geology
2014
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| Online Access: | http://hdl.handle.net/10092/9943 |