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...
Main Author: | |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
University of Canterbury. Geological Sciences
2014
|
Subjects: | |
Online Access: | https://dx.doi.org/10.26021/7944 https://ir.canterbury.ac.nz/handle/10092/9660 |