Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/72746
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dc.contributor.authorThomson, DFen_US
dc.date.accessioned2013-10-23T20:01:01Z-
dc.date.issued1990en_US
dc.identifier.govdocCR1990-0378en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/72746en_US
dc.description.abstractNo anomalous geochemical results obtained. The general model was that a magnetic high corresponded to a zone of shallow basement 2-4km in width trending 325 to 330 degrees controlled by major NW trending structures. This ridge was thought to be a basement high (paleo-topographic high) perhaps modified by minor re-activation of the controlling structures.en_US
dc.titleFinal report EL 5580 Tipperaryen_US
dc.relation.isatmap100Batchelor 5171en_US
dc.relation.isatmap100Tipperary 5170en_US
dc.relation.isatmap250Pine Creek SD5208en_US
dc.relation.isatgeolprovincePine Creek Orogenen_US
dc.identifier.tenureEL5580en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory21/04/2005en_US
dc.description.modifyhistory24/10/2006en_US
dc.description.modifyhistory09/02/2015en_US
dc.contributor.holderNewmont Australiaen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1990en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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