Wairakite, the calcium analogue of analcime, a new zeolite mineral
- 1 September 1955
- journal article
- Published by Mineralogical Society in Mineralogical Magazine and Journal of the Mineralogical Society
- Vol. 30 (230), 691-698
- https://doi.org/10.1180/minmag.1955.030.230.02
Abstract
During the study of hydrothermal alteration of cores recovered Dfrom holes drilled at Wairakei during the exploration for geothermal steam, an unusual zeolite mineral was found. Optical, chemical, and X-ray data indicate that this zeolite is a new mineral, the calcium analogue of analcime. The name wairakite is given to the new mineral after the locality Wairakei in New Zealand. Wairakei is situated in the central part of the North Island, approximately 4 miles north-north-east from Lake Taupo, in an active volcanic region. The material was submitted to Dr. D. S. Coombs, Department of Geology, University of Otago, Dunedin, for an investigation of its X-ray crystallography.Keywords
This publication has 3 references indexed in Scilit:
- Hydrothermal rock alteration at Wairakei, New ZealandEconomic Geology, 1953
- 481. Ion–exchange and ion-sieve processes in crystalline zeolitesJournal of the Chemical Society, 1950
- On sulphatic cancrinite and analcime (eudnophite) from Loch Borolan, AssyntMineralogical Magazine and Journal of the Mineralogical Society, 1941