Petrology of the gabbro and sheeted basaltic intrusives at North Cape, New Zealand
The North Cape massif consists of a semiconformable sequence of serpentinite, gabbro, sheeted sill and dike units, and pillow lavas. Although structurally disrupted, they can be interpreted in terms of an idealised ophiolite sequence and represent the most complete sequence in the Northland Ophiolit...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Royal Society Of New Zealand
1996
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Online Access: | http://hdl.handle.net/2292/4852 |