Abstract
Abstract Alunite has been noted as a common member of hydrothermal assemblages resulting from the epigene sulphuric acid alteration of acidic volcanic rocks (Steiner, 1953, 1963; Harvey, 1967). Although alunite is not uncommon in sinter deposits at Whitianga (Harvey, 1967) and in silicified andesite at Thames (Hutton, 1947), this is the first occurrence for the Coromandel Peninsula where the alunite occurs in silicified greywacke.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.