Contents
- TITLE_SECTIONTitle Section
- CHAPTERGeology of the Red Hill Complex, Nelson, New Zealand
- ILLUSTRATIONFig. 1.—Geological outline of the Nelson Ultramafic Belt. Inset shows the area discussed in this paper.
- ILLUSTRATIONFig. 2.—Idealised columns illustrating correlations of lithological units in Waterhouse (1964), Lauder (1965), and th...
- ILLUSTRATIONFig. 3.—Classification used in this paper for rocks composed of olivine, orthopyroxene, and clinopyroxene.
- ILLUSTRATIONGEOLOGICAL MAP OF THE RED HILL COMPLEX NELSON
- ILLUSTRATIONFig. 1.—Protoclastic texture in harzburgite. Note rounded porphyroclasts and fragmental matrix.
- ILLUSTRATIONFig. 2.—Partly recrystallised protoclastic harzburgite. Note smooth margins of some grains and remnants of matrix.
- ILLUSTRATIONFig. 1.—Irregular olivine grain in a completely recrystallised harzburgite.
- ILLUSTRATIONFig. 2.—Poikilitic or poikiloblastic orthopyroxene containing olivine grains. Most olivine grains within the crystal ...
- ILLUSTRATIONFig. 1.—Foliation defined by feldspar grains in a zone on either side of a vein composed of discontiguous diopside gr...
- ILLUSTRATIONFig. 2.—Laminated harzburgite. Lamination defined, at least in part, by subparallel, closely spaced veins of orthopyr...
- ILLUSTRATIONFig. 1.—Laminated harzburgite and dunite (light coloured) layers.
- ILLUSTRATIONFig. 2.—Intersecting layered structures. The later layering dipping to the right is referred to as metamorphic layering.
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