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The Sydney Basin and frozen prawns - the cool mineral connection

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conference contribution
posted on 2024-11-13, 12:42 authored by Paul CarrPaul Carr, Brian JonesBrian Jones, Bruce Selleck
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.

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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.

Pagination

9-13

Language

English

RIS ID

16624

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