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dc.contributor.authorWetherley, Cen_US
dc.date.accessioned2019-11-14T22:36:46Z-
dc.date.issued2019en_US
dc.identifier.govdocCR2019-0221en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/89497-
dc.description.abstractThis collaborative funding application was approved to drill two diamond holes for 1050 metres, in the Rover area southwest of the Tennant Creek Mineral Field. The Rover area has been the subject of exploration targeting for Tennant Creek style Cu-Au-Bi mineralisation since work by Peko in the mid 1970's. Todd River Resources (TRR) has tenure to the immediate southeast of the Rover 1 deposit, ground which last saw exploration activity by Western Desert Resources in 2012. Tenure is now with Todd River Resources Limited's subsidiary Todd River Metals Pty Ltd, and a program has been outlined for early 2019. EL 25581 covers much of the Rover field to the south and east of Rover 1 (Figure 1). Holes drilled through Wiso Basin cover and into the Warramunga Formation, which is the host sequence of both the known Rover mineralisation and all of the Tennant Creek Au-Cu-Bi deposits. This is an area with no surface exposure of the targeted sequence. The package being targeted has 70-200 metres of Wiso Basin cover under thin Tertiary/Quaternary sand cover, and so surface sampling is not effective. All exploration activity to date has been driven by geophysics and then requires drill testing. Geophysical interpretation of the area to date has outlined a complex package of the prospective sequence, with numerous offsetting faults and a number of both mafic and granitic intrusives. Target zones are small discrete magnetic highs, as well as gravity/density high zones with some magnetic signatures but density anomalies can also be targets as some deposits have no magnetite. The existing magnetics and gravity surveys (completed by WDR) were reprocessed in 2018 and targets generated for drill testing. RVDD0001 was drilled to 492.4m and RVDD0002 was drilled to 545.6m. Both holes sufficiently tested the modelled targets and were drilled through Wiso Basin sediments into the Warramunga Formation. Assay results were not exceptional, but follow-up exploration is warranted across the region.en_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationZincen_US
dc.subject.classificationLeaden_US
dc.subject.classificationCopperen_US
dc.subject.classificationPrecious metalsen_US
dc.subject.classificationGolden_US
dc.subject.classificationGeologyen_US
dc.subject.classificationRegional geologyen_US
dc.subject.classificationLocal geologyen_US
dc.subject.classificationMineralisationen_US
dc.subject.classificationPrevious explorationen_US
dc.subject.classificationDrillingen_US
dc.subject.classificationDiamond drillingen_US
dc.subject.classificationDrill collarsen_US
dc.subject.classificationDrill hole logsen_US
dc.subject.classificationDrill hole dataen_US
dc.subject.classificationMagnetic propertiesen_US
dc.subject.classificationMagnetic susceptibilityen_US
dc.subject.classificationDown hole geophysicsen_US
dc.subject.classificationDrill core samplingen_US
dc.subject.classificationAssayingen_US
dc.subject.classificationAssay valueen_US
dc.titleRover Project EL 25581 Drilling Collaboration Reporten_US
dc.relation.isatmap100Chaluba 5657en_US
dc.relation.isatmap250Bonney Well SF5302en_US
dc.relation.isatgeolprovinceWiso Basinen_US
dc.relation.isatgeolprovinceWarumpi Provinceen_US
dc.description.stratnameWarramunga Formationen_US
dc.description.geochemicalsampling314 Drill samplesen_US
dc.description.drilling2 Diamond holes for 1,038 m including 185.5 m of RC pre-collar (RVDD0001, RVDD0002)en_US
dc.identifier.tenureEL25581en_US
dc.description.modifyhistory30/03/2020en_US
dc.contributor.holderTodd River Metalsen_US
dc.contributor.holderTodd River Resourcesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)-
dc.identifier.govdocprefixCR2019-
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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