Please use this identifier to cite or link to this item:
Export to Endnote
https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/72734
Export to Endnote
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Creagh, CJ | en_US |
dc.date.accessioned | 2013-10-23T20:00:15Z | - |
dc.date.issued | 1990 | en_US |
dc.identifier.govdoc | CR1990-0336 | en_US |
dc.identifier.uri | https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/72734 | en_US |
dc.description.abstract | Work during the first year of the licence has concentrated on the acquisition and interpretation of regional magnetics, radiometrics. The interpretation has highlighted several features a) a linear N-NW magnetic high defining the eastern margin of the Pine Creek Shear Zone. b) A major NNW trending structure 25km east of and parallel to the Pine Creek Shear. c) Intersections of major NNW trending structure by NE trending lineaments. One significant anomaly has been identified within the licence. | en_US |
dc.description.abstract | Results from TM imagery and radiometric surveys not included within the report. | en_US |
dc.title | Annual Report Compass Creek 22-3-89 - 21-3-90. | en_US |
dc.relation.isatmap100 | McKinlay River 5271 | en_US |
dc.relation.isatmap250 | Pine Creek SD5208 | en_US |
dc.relation.isatgeolprovince | Pine Creek Orogen | en_US |
dc.identifier.tenure | EL6443 | en_US |
dc.description.modifyhistory | 02/10/2003 | en_US |
dc.description.modifyhistory | 01/03/2005 | en_US |
dc.description.modifyhistory | 21/04/2005 | en_US |
dc.description.modifyhistory | 24/10/2006 | en_US |
dc.description.modifyhistory | 09/02/2015 | en_US |
dc.contributor.holder | Billiton | en_US |
dc.identifier.collectionname | Minerals Exploration Reports (MEX) | en_US |
dc.identifier.govdocprefix | CR1990 | en_US |
local.flag.notified | 1 | |
Appears in Collections: | Minerals Exploration Reports (MEX) |
Files in this Report:
File | Size | Format | Add to Download |
---|---|---|---|
CR19900336.pdf | 1.12 MB | Add |
Items in GEMIS are protected by copyright unless otherwise indicated.