Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/65931
Export to Endnote
Full metadata record
DC FieldValueLanguage
dc.date.accessioned2013-10-23T11:03:19Z-
dc.date.issued1989en_US
dc.identifier.govdocCR1989-0130en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/65931en_US
dc.description.abstractThe original purpose of the EL was to sample and assess a claypan located in about the centre of the area for diamond indicators by means of several percussion drill holes to about 26 or 30 metres. This will give samples which are uncontaminated by material carried in by the wind and water flow from outside. Research of existing data indicated a strong magnetic anomaly associated with and slightly to the north west of the claypan, and ground. Surveys were conducted to locate and detail this anomaly. Altogether a total of ninteen kilometres of traverse was measured, (total field magnetic variations) over an area comprised of light mulga scrub and spinifex. The survey showed however that the anomaly was infact further to the north than anticipated and certainly not associated with the claypan. As a result the project has two targets for sampling; The calypan and the magnetic anomaly and environs. Also, with the magnetic anomaly being located so close to the northern boundary of the EL, it was necessary to lodge an application for an additional area (EL 6108 - Granted 29/08/1988). This will facilitate testing of the site and the area to the north.Following the identification of the magnetic anomaly a detailed survey was conducted measuring the vertical component of the magnetic field over an area of 300 metres x 200 metres. This showed the source to be located in a flat area of mulga scrub and red clayey loam with no outcroping rocks. A small test pit (300mm x 600mm) was dug at a grid reference 925N x 800E through 300mm of alluvium, and a sample of underlying weathered rock was taken from a depth of 400 to 500mm. THis proved to be banded ironstone formation with high magnetic susceptability. To date no test results are on hand for the sample and this will be included in next years report.en_US
dc.subject.classificationDiamondsen_US
dc.subject.classificationPitsen_US
dc.subject.classificationRock chip samplingen_US
dc.titleEL 5608 Report for the year ended 26.11.87 Year 1.en_US
dc.relation.isatmap100Doreen 5153en_US
dc.relation.isatmap250Mount Doreen SF5212en_US
dc.relation.isatgeolprovinceAileron Provinceen_US
dc.description.geochemicalsamplingRock chip samples collected from pit but results not on hand. Will be lodged in next years annual report.en_US
dc.description.mineprospectnameCoonegaen_US
dc.identifier.tenureEL5608en_US
dc.description.modifyhistory27/04/2005en_US
dc.description.modifyhistory15/01/2007en_US
dc.description.modifyhistory10/09/2009en_US
dc.description.modifyhistory12/08/2015en_US
dc.description.modifyhistory09/08/2023en_US
dc.contributor.holderJohannsen, LAen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1989en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

Files in this Report:
File SizeFormat Add to
Download
CR19890130.pdf218.1 kBPDF Add


Items in GEMIS are protected by copyright unless otherwise indicated.

Get Adobe Reader