Ordovician-Silurian boundary in Victoria and New South Wales, Australia

A. H M Vandeberg, B. D. Webby

Research output: Contribution to journalArticlepeer-review

4 Citations (Scopus)

Abstract

The late Ordovician and early Silurian is often represented by an unconformity or otherwise by beds bearing graptolies: no significant shelly faunas are known. In Darraweit Guium, Victoria, and in the Forbes-Parkes area of New South Wales, there may be beds spanning the Ordovician-Silurian boundary without a break, but nowhere have both the persculptus and acuminatus Zones been found in a single, structurally uncomplicated, succession. -Authors

Original languageEnglish
Pages (from-to)183-190
Number of pages8
JournalBulletin - British Museum (Natural History), Geology Series
Volume43
Publication statusPublished - 1988
Externally publishedYes

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