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Cambrian stratigraphy of the St. Valentines Peak area, north-western Tasmania

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Jago, JB and Pike, GA and Mills, D (1975) Cambrian stratigraphy of the St. Valentines Peak area, north-western Tasmania. Papers and Proceedings of the Royal Society of Tasmania, 109. pp. 85-90. ISSN 0080-4703

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Abstract

An important Late Middle Cambrian fossil locality occurs 2 km west of St.
Valentines Peak in north-western Tasmania. The Cambrian rocks to the north and west
of St. Valentines Peak are exposed in the core of the north-south trending St.
Valentines Peak Anticline. In the best exposed section (3 km north of the main fossil
locality), the oldest Cambrian unit is a massive, cherty, pyritic meta-sandstone and
meta-siltstone at least 100 m thick. This is overlain by 100 m of rhyolitic welded
tuff, 75 to 100 m of meta-sandstones and meta-siltstones, 100 m of a possible contact
metasomatic rock and 230 to 375 m of a pale grey chert which in turn is overlain by
about 17 m of fine breccia and poorly fossiliferous siltstone. This sequence is overlain
with probable disconformity by the basal chert conglomerate of the essentially
Ordovician Junee Group. It is suggested that the sediments of the main fossiliferous
locality occur stratigraphically below the section noted above. The Cambrian and
Ordovician rocks are intruded by Devonian granite and partly overlain by Tertiary
basalt.

Item Type: Article
Keywords: Tasmania, Hobart, Royal Society of Tasmania, RST, Van Diemens Land, natural history, science, ecology, taxonomy, botany, zoology, geology, geography, papers & proceedings, Australia, UTAS Library
Journal or Publication Title: Papers and Proceedings of the Royal Society of Tasmania
Page Range: pp. 85-90
ISSN: 0080-4703
Collections: Royal Society Collection > Papers & Proceedings of the Royal Society of Tasmania
Additional Information:

Copyright Royal Society of Tasmania

Date Deposited: 23 May 2012 05:00
Last Modified: 18 Nov 2014 04:34
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