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

A. H M Vandeberg; B. D. Webby

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

A. H M Vandeberg, B. D. Webby

Research output: Contribution to journal › Article

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 language	English
Pages (from-to)	183-190
Number of pages	8
Journal	Bulletin - British Museum (Natural History), Geology Series
Volume	43
Publication status	Published - 1988
Externally published	Yes

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

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",

author = "Vandeberg, {A. H M} and Webby, {B. D.}",

year = "1988",

language = "English",

volume = "43",

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AU - Vandeberg, A. H M

AU - Webby, B. D.

PY - 1988

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N2 - 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

AB - 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

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VL - 43

SP - 183

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JO - Bulletin - British Museum (Natural History), Geology Series

JF - Bulletin - British Museum (Natural History), Geology Series

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