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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/59768
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dc.contributor.authorSwarbrick, EEen_US
dc.date.accessioned2013-10-23T03:47:28Z-
dc.date.issued1968en_US
dc.identifier.govdocCR1968-0022en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/59768en_US
dc.description.abstractThe magnetic anomaly lies on a fault plane and is considered to be derived from magnetite mineralisation No other economic mineralisation is considered likely on the prospect. It was relinquished.en_US
dc.subject.classificationDeformation (structural geology)en_US
dc.subject.classificationFaultsen_US
dc.subject.classificationFaultingen_US
dc.subject.classificationGeological mappingen_US
dc.subject.classificationGeological environmenten_US
dc.subject.classificationGeological structuresen_US
dc.subject.classificationEvaluationen_US
dc.title1968 Report on the AP 1760 Mount Porteren_US
dc.relation.isatmap100Pine Creek 5270en_US
dc.relation.isatmap250Pine Creek SD5208en_US
dc.relation.isatgeolprovincePine Creek Orogenen_US
dc.description.stratnameGolden Dyke Formationen_US
dc.description.stratnameCullen Graniteen_US
dc.description.stratnameMasson Formationen_US
dc.description.stratnameBurrell Creek Formationen_US
dc.description.mineprospectnameMount Porteren_US
dc.identifier.tenureAP1760en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory29/01/2004en_US
dc.description.modifyhistory25/10/2016en_US
dc.description.modifyhistory28/09/2021en_US
dc.contributor.holderGeopekoen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1968en_US
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