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dc.contributor.authorWright, Pen_US
dc.date.accessioned2013-10-23T13:59:51Z-
dc.date.issued1989en_US
dc.identifier.govdocCR1989-0465en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/68087en_US
dc.description.abstractA geophysical interpretation was made on the data that was purchased by Metana from Austirex International Limited. An airborne geophysical survey was conducted by Austirex between June & July 1984. The flight lines were spaced by 200 metres, with tie lines separated by 4000 metres. A proton precession magnetometer was used for data collection. This had a resolution of 0.1 nano Tesla, a cycle rate of 0.5 seconds and a sample interval of 30 metres. The interpretation shown on figure 4 indicates that the leases are situated on west north west striking magnetic units. A parallel structural break crosses the north eastern part of the project area, with a fold in the magnetic units on the north eastern side of the fault. There are no obvious 'bulls eye' type magnetic anomalies within the leases. A ground magnetic survey was carried out by Solo Geophysics, over Mineral Claims 388 to 398. Readings were taken at a height of 8 feet at 5 metre intervals along 40 metre spaced grid lines. The contoured results are not given, as the surface noise obviously dominated the stacked profiles. The survey does not reveal any likely magnetic ironstone source. Soil samples were taken on an 160 x 40 metre spaced pattern. From orientation work elsewhere in the Tennant Creek field the optimum size fraction for sampling soil for gold was found to be -180 microns. Samples of this size fraction were submitted for aqua regia/GTA gold analysis only. The maximum assays are spot highs up to 16 ppb against a background of less than 2 ppb. The aeromagnetic interpretation and results from the ground magnetic survey do not suggest the presence of a massive, magnetite/hematite body. Future exploration should include bedrock geochemistry drilled in traverses across all, or selected parts of the lease to determine the underlying lithology and to investigate the potential for shallow mineralisation. Care must be taken to drill to bedrock as the laterite may mask the underlying geochemistry. From experience elsewhere in the Tennant Creek field it is recommended that samples be analysed for selected base metals as well as for gold. Rock chip sampling is also recommended, including samples of laterite.en_US
dc.subject.classificationGold explorationen_US
dc.subject.classificationSoil samplingen_US
dc.subject.classificationMagnetic surveysen_US
dc.subject.classificationGeophysical interpretationen_US
dc.subject.classificationGeological mappingen_US
dc.titleExploration summary report Little Ben period ending 01-03-1989.en_US
dc.relation.isatmap100Tennant Creek 5758en_US
dc.relation.isatmap250Tennant Creek SE5314en_US
dc.relation.isatgeolprovinceTennant Regionen_US
dc.description.stratnameCarraman Formationen_US
dc.description.stratnameBlack Eye Memberen_US
dc.description.geochemicalsamplingSoil sampling took place but no results were given.en_US
dc.description.mineprospectnameLittle Benen_US
dc.identifier.tenureMCC408en_US
dc.identifier.tenureMCC409en_US
dc.identifier.tenureMCC410en_US
dc.identifier.tenureMCC411en_US
dc.identifier.tenureMCC412en_US
dc.identifier.tenureMCC387en_US
dc.identifier.tenureMCC389en_US
dc.identifier.tenureMCC390en_US
dc.identifier.tenureMCC391en_US
dc.identifier.tenureMCC392en_US
dc.identifier.tenureMCC393en_US
dc.identifier.tenureMCC394en_US
dc.identifier.tenureMCC395en_US
dc.identifier.tenureMCC396en_US
dc.identifier.tenureMCC397en_US
dc.identifier.tenureMCC398en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory22/04/2005en_US
dc.description.modifyhistory15/01/2007en_US
dc.description.modifyhistory08/05/2009en_US
dc.description.modifyhistory12/08/2015en_US
dc.contributor.holderMetana Mineralsen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1989en_US
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Appears in Collections:Minerals Exploration Reports (MEX)

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