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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/70869
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dc.contributor.authorPatterson, GWen_US
dc.date.accessioned2013-10-23T17:47:02Z-
dc.date.issued1964en_US
dc.identifier.govdocCR1964-0022en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/70869en_US
dc.description.abstractThe existence of a narrow zone of anomalous lead soil values about 7,000 feet long, outlined by A.H. Debnam in 1955 as anomalies A and B, has been definitely established. The anomalies undoubtedly represent conformable lead mineralisation in steeply dipping siltstone, an extension of the lead occurrences 2 miles to the southeast, tested by costeaning and drilling during 1954-55. Such a well defined zone presents a good drilling target and three inclined diamond drill holes totalling 1,000 feet should be sufficient to test the prospect.en_US
dc.subject.classificationLeaden_US
dc.subject.classificationSoil samplingen_US
dc.title1964 Geochemical Prospecting of Northern Lead Anomalies on AP 1130 Namoona, NTen_US
dc.relation.isatmap100Mundogie 5371en_US
dc.relation.isatmap250Mount Evelyn SD5305en_US
dc.relation.isatgeolprovincePine Creek Orogenen_US
dc.description.geochemicalsamplingHundreds of soil samples were collected, the exact figure is unknown.en_US
dc.description.mineprospectnameNamoona Prospecten_US
dc.description.mineprospectnameAnomaly Aen_US
dc.description.mineprospectnameAnomaly Ben_US
dc.identifier.tenureAP1130en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory23/12/2009en_US
dc.description.modifyhistory25/11/2016en_US
dc.description.modifyhistory27/09/2021en_US
dc.contributor.holderCRA Explorationen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1964en_US
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