Fill compaction criteria for Port Hills Gravel Formation soils, Nelson
Port Hills Gravel Formation (PHG) is a Pliocene terrestrial soil-like deposit. It is located in Nelson as part of the Marsden and Port Hills Synclines. PHG is comprised of heterogeneous clay and silt bound gravel, with lenses of sandstone and occasional lignite seams and is intersected by northeast...
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| Language: | en |
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University of Canterbury. Geological Sciences
2010
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| Online Access: | http://hdl.handle.net/10092/4387 |