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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/131155
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dc.contributor.authorLove, R. J.-
dc.coverage.spatialAdelaide Geosyncline, Mt Lofty Ranges, South Australia-
dc.date.issued1972-
dc.identifier.urihttp://hdl.handle.net/2440/131155-
dc.descriptionThis item is only available electronically.en
dc.description.abstractLate Precambrian sediments, in the vicinity of Sturt Gorge, have been mapped and investigated geochemically. The sequence consists of 112 metres of tillite and interbedded arenites (Sturt Tillite) overlain by about 2000 metres of finely laminated shales (Tapley Hill Formation). A combination of geochemical and stratigraphic observations suggested that silts derived from the till matrix were transported into a shallow marine basin by the process of glacial outwash.en
dc.language.isoenen
dc.subjectHonours; Geology; Late Precambrian; Tapley Hill Formation; Sturt Tillite; stratigraphy; geochemistry; depositional environmentsen
dc.titleThe geochemistry of the Tapley Hill Formation and Sturt Tillite, near Darlington, South Australiaen
dc.typeThesisen
dc.contributor.schoolSchool of Physical Sciencesen
dc.provenanceThis electronic version is made publicly available by the University of Adelaide in accordance with its open access policy for student theses. Copyright in this thesis remains with the author. This thesis may incorporate third party material which has been used by the author pursuant to Fair Dealing exceptions. If you are the author of this thesis and do not wish it to be made publicly available, or you are the owner of any included third party copyright material you wish to be removed from this electronic version, please complete the take down form located at: http://www.adelaide.edu.au/legalsen
dc.description.dissertationThesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1972-
Appears in Collections:School of Physical Sciences

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