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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/128253
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dc.contributor.authorKay, B. V.-
dc.coverage.spatialCurnamona Province, South Australia, New South Wales-
dc.date.issued2017-
dc.identifier.urihttp://hdl.handle.net/2440/128253-
dc.descriptionThis item is only available electronically.en
dc.description.abstractIn July 2017, scale-reduction was undertaken to improve the bandwidth and resolution of the AusLAMP defined Curnamona Conductor (Robertson et al., 2016) by way of a broadband magnetotelluric profile with site spacing of 2 km, extending from the Erudina Domain across the Mudguard and Quinyambie Domains in the Curnamona Province. A fossil fluid pathway has been identified from the lower mid crustal conductor to the near surface situated near a topographic basement high. The upper crustal conductor has been further delineated beneath the Quinyambie Domain to within 5 km of the surface situated alongside a major crustal feature.en
dc.language.isoenen
dc.subjectHonours; Geology; magnetotellurics; crustal fluid; UNCOVER; Curnamona conductor; scale-reductionen
dc.titleTesting the uncover paradigm: crustal fluid pathways in the Curnamona Provinceen
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, 2017-
Appears in Collections:School of Physical Sciences

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