Test environment running 7.6.6

Cultural advice

The Australian National University acknowledges, celebrates and pays our respects to the Ngunnawal and Ngambri people of the Canberra region and to all First Nations Australians on whose traditional lands we meet and work, and whose cultures are among the oldest continuing cultures in human history.

Aboriginal and Torres Strait Islander peoples are advised that ANU Library collections may include images, names, voices, and other representations of deceased persons.

Material in the collection may contain terms, language or views that reflect the period in which the item was created and may be considered inappropriate today.

FACIES OF ORE FORMATION

Thumbnail Image

Date

1979

Authors

Journal Title

Journal ISSN

Volume Title

Publisher

Abstract

The Pegmont deposit is a stratiform Pb-Zn sulphide body occurring in a thin, iron-rich metasedimentary unit situated near the top of the Kuridala Formation, a part of the Mary Kathleen group of the Middle Proterozoic ″Eastern Geosyncline″ succession of the Mount Isa-Cloncurry district. It is suggested that in regions of known or suspected stratiform ore occurrence small iron-rich sedimentary units should be examined with the concept of ″facies of ore formation″ in mind, and any highly localized development of high grade regional metamorphic mineral assemblages should be investigated as potential envelopes of ore.

Description

Keywords

Citation

URI

https://dspace-test.anu.edu.au/handle/1885/733744314

Collections

DevOps Pure Testing

Source

Proceedings - Australasian Institute of Mining and Metallurgy

Type

Article

Book Title

Entity type

Access Statement

License Rights

DOI

Restricted until

DSpace software copyright © 2002-2026 LYRASIS