Calcite pseudomorphs after ikaite (glendonite) are common in the Permian marine sequences of the Sydney Basin and have been recorded from more than 30 localities representing six major glenonite-forming intervals. Recognition of glenonites in Sydney Basin strata provides unequivocal evidence for coldwater deposition.
History
Citation
Carr, P. F., Jones, B. G. & Selleck, B. (2006). The Sydney Basin and frozen prawns - the cool mineral connection. In A. C. Hutton & J. Griffin (Eds.), Advances in the Study of the Sydney Basin (pp. 9-13). Wollongong: School of Earth & Environmental Sciences.