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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Bibliographic Details
Main Author: Win, Noel Antony
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