Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/83895
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dc.contributor.authorDaily, B.en
dc.contributor.authorMilnes, A.en
dc.date.issued1971en
dc.identifier.citationTransactions of the Royal Society of South Australia, 1971; 95(4):199-214en
dc.identifier.issn0376-2750en
dc.identifier.issn0372-1426en
dc.identifier.urihttp://hdl.handle.net/2440/83895-
dc.description.abstractHyolithids and other Lower Cambrian fossils occur within marbles in low-stage metamorphic rocks (Forktree Limestone and Heatherdale Shale) forming the core of a north-east plunging regional anticline, overturned to the south-east. A great thickness of partially bioturbated Kanmantoo Group metasediments, dominantly clastics, but including sulphide-rich calc-phyllites of the Talisker Calc-siltstone, conformably overlie the Heatherdale Shale. The rapidly deposited elastics, including numerous thin conglomerates, are interpreted as products of the Kangarooian Movements known to have affected the region now occupied by Investigator Strait and Gulf St. Vincent. The newly proposed stratigraphic subdivision for that part of the Group discussed should lead to a more reliable picture of the occurrence and the relationships of these rocks to other sequences within the Mt. Lofty Ranges and Kangaroo Island.en
dc.description.statementofresponsibilityB. Daily and A. R. Milnesen
dc.language.isoenen
dc.rightsCopyright status unknownen
dc.titleStratigraphic notes on the Lower Cambrian fossiliferous sediments between Campbell Creek and Tunkalilla Beach in the type section of the Kanmantoo Group, Fleurieu Peninsula, South Australiaen
dc.typeJournal articleen
dc.identifier.rmid0030019535en
dc.identifier.pubid166432-
pubs.library.collectionGeology & Geophysics publicationsen
pubs.library.teamDS04en
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
Appears in Collections:Geology & Geophysics publications

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