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dc.contributor.authorParker, BJen_US
dc.contributor.authorRussell, SCen_US
dc.date.accessioned2017-01-22T22:51:20Z-
dc.date.issued2005en_US
dc.identifier.govdocCR2005-0270en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/84179en_US
dc.description.abstractThis report records the exploration work completed on EL 23284 during its second year of tenure, from 14 July 2004 to 15 July 2005. Targets are shallow haematite-ironstone related gold deposits. Several granted Mineral Claims and Leases are located within Exploration Licence 23284. These are located on the southern boundary of the Licence area and extend east and west. Exploration activities within these tenements are subject to individual tenement reports and will not be reported in this Annual Report. Exploration conducted on the remaining area outside of the Mineral Claims and Leases in Exploration Licence 23284 is reported. 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 detailed gravity survey conducted within EL 23284 as part of a broader, regional survey covering most of the Chariot Mineralised Corridor has identified several low-order residual bouguer gravity anomalies which require detailed modelling prior to further exploration. The projected surface positions for two analytic signal magnetic anomalies (Analytic 1-2) were visited during the year. No outcrop was identified at either site and the causative bodies remain unexplained. It appears that the magnetic anomalies are quite deep (>150m vertical) however detailed modelling is required to confirm this. The fact that non-magnetic ironstones, hosting gold mineralisation are known to exist (Chariot and Malbec West 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.classificationBase metalsen_US
dc.subject.classificationGravity dataen_US
dc.subject.classificationGravity anomaliesen_US
dc.subject.classificationMagnetic anomaliesen_US
dc.subject.classificationReconnaissanceen_US
dc.subject.classificationMine managementen_US
dc.subject.classificationData compilationen_US
dc.subject.classificationGeologyen_US
dc.subject.classificationRegional geologyen_US
dc.subject.classificationGeneral geologyen_US
dc.titleEL 23284 Corridor 1 Second annual report 16 July 2004 to 15 July 2005en_US
dc.relation.isatmap100Tennant Creek 5758en_US
dc.relation.isatmap250Tennant Creek SE5314en_US
dc.relation.isatgeolprovinceTennant Regionen_US
dc.description.stratnameWarramunga Formationen_US
dc.description.mineprospectnameCorridoren_US
dc.description.mineprospectnameCharioten_US
dc.description.mineprospectnameTC8en_US
dc.identifier.tenureEL23284en_US
dc.description.modifyhistory11/11/2013en_US
dc.description.modifyhistory10/01/2017en_US
dc.contributor.holderGiants Reef Explorationen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2005en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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