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dc.contributor.authorJenkins Den_US
dc.contributor.authorPoynton Cen_US
dc.date.accessioned2017-10-12T22:56:52Z-
dc.date.issued2008en_US
dc.identifier.govdocCR2008-0505en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/86475en_US
dc.description.abstractEL 25688 Mountain Creek is in the West McArthur Basin, Northern Territory of Australia, entirely within the proposed Limmen National Park. It is about 40 kilometres south of the Roper River. The geology of the area is comprised of Proterozoic sandstones, siltstones and mudstones of the Moroak Sandstone, Velkerri , Kyalla Member and Chalmers River Formation. These are overlaid locally by Cambrian Antrim Plateau Volcanics and intruded by Proterozoic dolerite and diorite. The exploration objective was either an Unconformity-type Uranium Deposit similar to those of the Alligator River Province, or a palaeochannel deposit similar to the Honeymoon Well project in South Australia. In the Unconformity-type deposits, the uranium is associated with chloritised sandstone, while the palaeochannel deposits rely on uranium fixation by change of oxidation state with organic material. A review of available open-file information on the license was performed, seeking evidence to facilitate the exploration for uranium within the area. The most readily accessible data was airborne geophysics, geological mapping, mineral occurrence and topographic information. Airborne radiometric anomalies have been investigated on the ground, using a portable gamma ray spectrometer, an Exploranium GR135 Plus, and have been sampled for analysis where of interest. Most of the anomalies were associated with black soils, though two of them correlated with lateritic duricrust outcrops. Determinations of uranium, thorium and potassium were made using the gamma ray spectrometer, while rock chip samples were also investigated with a Niton field-portable XRF device. Soil geochemical samples were taken in areas that lacked outcrop, and submitted for ICP-MS multi-element assay. The reconnaissance ground radiometric and geochemical survey has shown that the airborne radiometric anomalies were mostly in brown and black soils. The uranium and thorium abundances were determined by ICP-MS to be a maximum of 5.54ppm for U and 7ppm for Th.en_US
dc.subject.classificationUraniumen_US
dc.subject.classificationThoriumen_US
dc.subject.classificationGeologyen_US
dc.subject.classificationRegional geologyen_US
dc.subject.classificationReviewsen_US
dc.subject.classificationDataen_US
dc.subject.classificationGeophysicsen_US
dc.subject.classificationReconnaissanceen_US
dc.subject.classificationSpectrometersen_US
dc.subject.classificationX ray fluorescence spectrometersen_US
dc.subject.classificationSamplingen_US
dc.subject.classificationSoil samplingen_US
dc.subject.classificationRock chip samplingen_US
dc.titleAnnual report EL 25688 Mountain Creek NT to 23 September 2008en_US
dc.relation.isatmap100St. Vidgeon 5867en_US
dc.relation.isatmap250Hodgson Downs SD5314en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.description.stratnameMoroak Sandstone, Velkerri Formation, Kyalla Member, Chambers River Formationen_US
dc.description.geochemicalsampling1 Rock chip sampleen_US
dc.description.geochemicalsampling6 Soil samplesen_US
dc.description.mineprospectnameBuffaloen_US
dc.identifier.tenureEL25688en_US
dc.description.modifyhistory03/10/2008en_US
dc.description.modifyhistory13/10/2010en_US
dc.description.modifyhistory21/11/2013en_US
dc.description.modifyhistory17/08/2017en_US
dc.description.modifyhistory19/09/2017en_US
dc.description.modifyhistory13/10/2017en_US
dc.contributor.holderTerra Searchen_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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