Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/85493
Export to Endnote
Full metadata record
DC FieldValueLanguage
dc.contributor.authorEupene, GSen_US
dc.date.accessioned2017-06-15T03:59:48Z-
dc.date.issued2006en_US
dc.identifier.govdocCR2006-0493en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/85493en_US
dc.description.abstractEL 24520 was granted on the 3 October 2005 for a period of six years. During the first year of tenure work focused on literature search for data relating to EL 24520, report preparation. administrative duties, and planning for upcoming field season. The Target Area is situated within the Ashburton Province (1400-1700Ma), a sequence of unmetamorphosed and weakly deformed predominantly shallow marine sediments. The Ashburton Province overlies the Warramunga Province which is deformed by the Tennant Orogeny (1850Ma) and intruded by granites of the same age. The Ashburton Province is overlain by Palaeozoic sediments of the Georgina and Wiso basins to the east and west respectively. Previous exploration within the district has focused on the potential for diamonds and base metals but has been limited in extent because of the poorly developed drainage system and the extensive, but generally thin, alluvial and aeolian cover. The high proportion of Type 2 microdiamonds underpins the exploration potential of the area. Four of the twelve microdiamonds recovered from within the Project Area are un-resorbed octahedral forms (or parts thereof) and may be indicative of a proximal source. The remainder of the diamonds are irregular to cube shaped, pink-brown to cream in colour (Type 3). Follow-up of the microdiamond anomaly initially recognised by Ashton has been limited and there are probably a number of reasons for this. Follow-up by traditional gravel and loam sampling methods would have been hampered by poorly defined, low-energy, sand-choked drainages and the widespread presence of transported soil cover. Successful follow-up of the diamonds will require the application of geophysical techniques such as airborne magnetic, electromagnetic and gravity surveys. Analysis of these data will allow the identification of discrete targets within the zones of interest defined by the presence of anomalous concentrations of microdiamonds and will also aid in the delineation of old, buried creek beds. Sampling of palaeo-channels by auger drilling techniques can provide better quality samples in areas with poorly developed surface drainage as Crossland Mining has successfully demonstrated at some of its other project areas.en_US
dc.subject.classificationDiamondsen_US
dc.subject.classificationGeologyen_US
dc.subject.classificationExploration historyen_US
dc.subject.classificationReviewsen_US
dc.titleFirst annual report for EL 24520 Lake Woods Project 3 October 2005 to 2 October 2006en_US
dc.relation.isatmap100Elliott 5662en_US
dc.relation.isatmap100Helen 5661en_US
dc.relation.isatmap250Beetaloo SE5306en_US
dc.relation.isatmap250Helen Springs SE5310en_US
dc.relation.isatgeolprovinceTennant Regionen_US
dc.identifier.tenureEL24520en_US
dc.description.modifyhistory06/12/2006en_US
dc.description.modifyhistory05/08/2010en_US
dc.description.modifyhistory28/11/2013en_US
dc.description.modifyhistory11/05/2017en_US
dc.contributor.holderCrossland Minesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2006en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

Files in this Report:
File SizeFormat Add to
Download
EL24520_2006_A.pdf400.75 kBPDF Add


Items in GEMIS are protected by copyright unless otherwise indicated.

Get Adobe Reader