Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/103375
Type: Thesis
Title: Electrical structure analysis of Carrapateena and Wirrda Well prospects, Stuart Shelf, from integrated geophysical and drillcore data
Author: Low, J. K. B.
Issue Date: 2010
School/Discipline: School of Physical Sciences
Abstract: Magnetotelluric (MT) datasets from Carrapateena and Wirrda Well prospects were inverted to produce MT models with geophysical and drillcore data as constraints. MT is an excellent technique in mapping the distribution of prospective rocks shielded by thick layers of cover sequences. However, the causes for most enhanced conductivity anomalies remain poorly understood and would require further research and investigation. The MT model of Carrapateena detected three conductive anomalies distributed across the southeastern and western side of the survey area. The MT data were able to detect the ore body described by the drillcore logs and potential field surveys but was shown to be imaged at only the first 500-900m of the basement rocks. However, at greater depths, the anomaly deviated to the west of the survey area although the drillcore logs and potential field surveys indicated otherwise. The loss of conductivity is suggested to be due to the change in nature of the sulphides from interconnected sulphides to disseminated sulphides. In addition, both the western and southeastern anomalies imaged at a depth of 1km are hypothesized to be caused by shear zones from a northeast and a northwest trending fault. The MT model of Wirrda Well detected two enhanced electrical anomalies at the north and south of the survey region. The northern and southern anomalies were shown to have high conductivity despite having a low density contrast from the potential fields survey. The lack of drillcore logs within the vicinity of the anomalies prevented further understanding as to the cause of both anomalies. However, observation of a nearby drillcore log at WW02 suggested a low concentration of interconnected sulphides to be the cause of the anomaly. In summary, the results from this study suggested that the nature of the sulphides play an important role in causing enhanced electrical anomalies in an MT model. The results also indicate a possible detection of anomalies caused by mineralisation along shear zones. Therefore, MT may be a poor choice for detection of ore bodies on the Stuart Shelf but could potentially be useful in imaging pathways of mineralising fluids through faults or shear zones. This could be invaluable with further research to understand and investigate the formation of IOCG deposits. The lack of drillcore logs at the identified anomalies within Carrapateena and Wirrda Well however proved to be a limiting factor in achieving a solid conclusion for the proposed hypothesis described above.
Dissertation Note: Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
Where: Stuart Shelf, Adelaide Geosyncline, Gawler Craton, South Australia
Keywords: Honours; Geology; geophysical techniques, exploration, mineralisation
Description: This item is only available electronically.
Provenance: This 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/legals
Appears in Collections:School of Physical Sciences

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