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dc.date.accessioned2024-06-05T22:04:38Z-
dc.date.issued2024en_US
dc.identifier.govdocCR2023-0717en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/92941-
dc.description.abstractLate Paleoproterozoic rocks in northwest Queensland and the Northern Territory host world-class stratiform sediment-hosted Zn-Pb-Ag deposits. These orebodies occur in intracontinental rift or rifted margin (marine) basins. Host rocks to these deposits are carbonaceous and/or pyritic black and grey (dolomitic) siltstone, mudstone and shale, often with a significant clastic carbonate (dolomite) component. The same lithologies occur within the McArthur Basin which hosts the world class HYC deposit and the Walker River Project, ~300 km to the north. Mineralisation at HYC is in part controlled by the Batten Fault Zone, a prominent north-south aligned eastward-deepening half-graben (aka the Batten Fault Trough). The Walker Fault Trough, a north continuation of the Batten Fault Trough, hosts the Walker River Project. The lithological and structural settings for the Walker River Project are thought by NTGS and Geoscience Australia to be analogous to the HYC deposit. Economic stratiform sediment-hosted Zn-Pb-Ag deposits are often associated with recognisable residual gravity responses, either directly related to mineralisation or associated pyritic sediments. Gravity is therefore a primary exploration tool. Government gravity stations have been acquired over the project area at roughly a 4 km density and due to land access restrictions, only one 'exploration' gravity survey has been conducted on the project since the discovery of the Walker Gossan in 1972 (2.7% Pb from rock chip). The 2016 gravity survey consisted of 160 stations acquired on six widely spaced traverses at 100 m spacing. Despite these limitations three unexplained gravity and/or soils geochemical anomalies were identified in structurally favourable locations. The Walker River AGG survey (Figure 1) over the highly prospective project area has expedited the geological knowledge and the exploration potential of the area. Several targets of interest have been identified from the AGG survey. Due to the short survey duration, the airborne survey minimised the impact to the local community and negate the need for extensive ground gravity surveys (to acquire the equivalent coverage) and the precursor archaeological clearance campaign/s. Discussions with local communities over access to AGG features of interest will commence shortly.en_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationZincen_US
dc.subject.classificationLeaden_US
dc.subject.classificationPrecious metalsen_US
dc.subject.classificationSilveren_US
dc.subject.classificationGeophysical dataen_US
dc.subject.classificationGeophysical surveysen_US
dc.subject.classificationAerial geophysical surveysen_US
dc.subject.classificationAirborne Gravity Gradiometeren_US
dc.titleWalker River Airborne Gravity Gradiometry (AGG) surveyen_US
dc.relation.isatmap100Koolatong 6071en_US
dc.relation.isatmap100Blue Mud Bay 6070en_US
dc.relation.isatmap250Blue Mud Bay SD5307en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.relation.isatgeolprovinceArnhem Provinceen_US
dc.identifier.tenureEL385en_US
dc.identifier.tenureEL24305en_US
dc.identifier.tenureELA30956en_US
dc.description.modifyhistory12/02/2024en_US
dc.description.modifyhistory05/06/2024en_US
dc.description.modifyhistory04/04/2025en_US
dc.contributor.holderRio Tinto Explorationen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)
dc.identifier.govdocprefixCR2023
local.flag.notified1en
Appears in Collections:Minerals Exploration Reports (MEX)

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