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dc.contributor.authorRussell, SCen_US
dc.contributor.authorCahill, JLen_US
dc.date.accessioned2016-11-10T01:24:01Z-
dc.date.issued2004en_US
dc.identifier.govdocCR2004-0494en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/83624en_US
dc.description.abstractThis report records the exploration work completed on EL 23284 during its first year of tenure, from 14 July 2003 to 15 July 2004. Targets are shallow haematite-ironstone related gold deposits. During the first year a brief review of all current exploration information and opportunities within the licence area was completed. The location of the Chariot mine and TC8 gold mines to EL 23284 along the Chariot trend made this Exploration Licence a highly prospective target area due to its structural significance and probable complexity. Additionally the highly developed understanding of the local geology as a consequence of continued exploration on the Chariot resource, combined with the EL's location to existing mine infrastructure ranked this Licence area as a high priority exploration project area. The three magnetic anomalies (Analytic 1-3) are targets of interest and will be modelled to determine depth to body top during the next year. It appears that the magnetic anomalies are quite deep (>150m vertical) however detailed modelling is required to confirm this. A detailed gravity survey was conducted within EL 23284 as part of a broader, regional survey covering most of the Chariot Mineralised Corridor. Several low order bouguer gravity anomalies were identified within the Licence area. As part of the more regional exploration along the CMC the production of structural, geological and geochemical layers which can be interrogated within the Company's GIS database will continue during the next reporting period. The detailed gravity survey appears to have added a new dimension to Giants Reef's understanding of the non-outcropping geology and the distribution of non-magnetic ironstone bodies within the survey area. The fact that non-magnetic ironstones, hosting gold mineralisation are known to exist (Chariot and Malbec deposits), yet have not really been searched for previously in the Tennant Creek Goldfield, means that the potential for new discoveries is highly likely.en_US
dc.subject.classificationPrecious metalsen_US
dc.subject.classificationGolden_US
dc.subject.classificationIronstoneen_US
dc.subject.classificationLiterature reviewsen_US
dc.subject.classificationGeophysical surveysen_US
dc.subject.classificationMagnetic surveysen_US
dc.subject.classificationGravity surveysen_US
dc.subject.classificationGeophysical interpretationen_US
dc.subject.classificationBouguer anomaly mapsen_US
dc.subject.classificationGeologyen_US
dc.subject.classificationRegional geologyen_US
dc.subject.classificationGeneral geologyen_US
dc.titleEL 23284 Corridor 1 First annual report 16 July 2003 to 15 July 2004en_US
dc.relation.isatmap100Tennant Creek 5758en_US
dc.relation.isatmap250Tennant Creek SE5314en_US
dc.relation.isatgeolprovinceTennant Regionen_US
dc.description.mineprospectnameCharioten_US
dc.description.mineprospectnameTC8en_US
dc.identifier.tenureEL23284en_US
dc.description.modifyhistory16/03/2006en_US
dc.description.modifyhistory10/11/2016en_US
dc.contributor.holderGiants Reef Explorationen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2004en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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