Formation of Fe-rich subsurface precipitate layers on White Island, New Zealand
White Island is a highly active volcano with an acidic, S-rich hydrothermal system in the Bay of Plenty, North Island, New Zealand. In this acidic environment a series of subsurface Fe-rich layers are ubiquitous in the crater sediments at shallow depth and are capable of modifying the flow and gas f...
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Format: | Other/Unknown Material |
Language: | English |
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University of Canterbury. Geological Sciences
2014
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Online Access: | http://hdl.handle.net/10092/9660 https://doi.org/10.26021/7944 |