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dc.contributor.authorSeymour, KMen_US
dc.date.accessioned2013-10-24T03:29:06Z-
dc.date.issued2008en_US
dc.identifier.govdocCR2008-0280en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/74414en_US
dc.description.abstractGlengarry Resources' Rum Jungle Project is located 65km south of Darwin and 25km northeast of Batchelor along the Stuart Highway and Alice Springs to Darwin Railway line. The Project encompasses over 140km2 of prospective Proterozoic stratigraphy in the Pine Creek Geosyncline, proximal to the historical Rum Jungle Uranium Mine and the Woodcutters Lead-Zinc Mine. Rum Jungle produced 0.66M tonnes @ 0.43% U3O8 for 3530 tonnes U3O8 between 1954 and 1971. Approximately 6M tonnes @ 12% zinc and 6% lead was mined from the Woodcutters Mine between 1985 and 1999. Production of 17,800 tonnes @ 10.7g/t gold was also mined from three small Sundance pits in 1986 and 1993, located 2.5km east of Batchelor and 12km southwest of the Woodcutters Mine. Within the Rum Jungle Project the Manton River EL24971 abuts the eastern margin of the Archaean Rum Jungle Complex. The Complex is mapped as two subcropping domal inliers of Archaean schists and fractionated I plus S-type granite gneisses unconformably draped by Lower Proterozoic Manton Group and Mt Partridge Group metasediments of the Pine Creek Geosyncline. The age of the geosyncline is constrained between 2470 and 1870Ma. Multiple phases of folding and faulting affected the Pine Creek rocks between 1880 - 1760Ma resulting in gently folded northsouth trending stratigraphy. The sedimentary rocks have been metamorphosed to subgreenschist facies. The regionally extensive and northeast trending Giants Reef Fault truncates the Rum Jungle Complex and displays dextral strike slip faulting, displacing the Rum Jungle Complex up to 7km within the Manton River EL. Geology within the Manton River EL is dominated by older Crater Formation and Coomalie Dolostone overlain by Whites Formation metasediments along the western limb of the Woodcutters Anticline. The Whites Formation is dominated by pyritic carbonaceous shale and hosts the Rum Jungle uranium deposits plus base metal mineralisation at Woodcutters. The failure to secure a suitable drilling contractor during the year has severely hampered Glengarry's proposed exploration activities during the year. Exploration undertaken within EL 24971 by Glengarry Resources during the reporting period was therefore restricted to further reconnaissance rock chip sampling. No anomalous results were returned.en_US
dc.subject.classificationGold explorationen_US
dc.subject.classificationUranium explorationen_US
dc.subject.classificationBase metal explorationen_US
dc.subject.classificationRock chip samplingen_US
dc.titleAnnual report on EL 24971 Manton River, for the period 14 June 2007 to 13 June 2008en_US
dc.relation.isatmap100Noonamah 5172en_US
dc.relation.isatmap250Darwin SD5204en_US
dc.relation.isatgeolprovincePine Creek Orogenen_US
dc.description.stratnameCrater Formationen_US
dc.description.stratnameCoomalie Dolomiteen_US
dc.description.stratnameWhites Formationen_US
dc.description.geochemicalsamplingreconnaissance rock chip samplingen_US
dc.description.mineprospectnameMantonen_US
dc.description.mineprospectnameAcacia Southen_US
dc.identifier.tenureEL24971en_US
dc.description.modifyhistory09/07/2008en_US
dc.description.modifyhistory16/07/2009en_US
dc.description.modifyhistory07/06/2013en_US
dc.description.modifyhistory21/11/2013en_US
dc.contributor.holderGlengarry Resourcesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2008en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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