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  4. School of Physical Sciences
Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/115300
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dc.contributor.authorThiele, W. K.-
dc.coverage.spatialKanmantoo Trough, Fleurieu Peninsula, South Australia-
dc.date.issued1961-
dc.identifier.urihttp://hdl.handle.net/2440/115300-
dc.descriptionThis item is only available electronically.en
dc.description.abstractThe Nairne Pyrite Formation is a sedimentary sulphide deposit occurring near the base of the Kanmantoo series of rocks. The average sulphide content of the formation is 10%, half of which consists of pyrrhotite. The measurement of susceptibility and permanent remnant magnetism of the formation, ground magnetic surveys across the horizon, and the analysis of aeromagnetic maps covering the northern area of outcrop are described. The results obtained are discussed and some conclusions drawn on the applicability of magnetic prospecting to the search for this deposit.en
dc.language.isoenen
dc.subjectHonours; Geology; Kanmantoo Group; pyrite; pyrrhotite; magnetism; aeromagneticsen
dc.titleThe magnetics of the Nairne Pyrite Formationen
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, 1961-
Appears in Collections:School of Physical Sciences

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