Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/73673
Export to Endnote
Title: Annual report for EL 23684, 17 June 2005 to 16 June 2006
Title Holder / Company: Crossland Mines
Report id: CR2006-0213
Tenure: EL23684
Year: 2006
Author: Eupene, GS
Abstract: The Western Creek project (EL23684) is located 78km south west of Larrimah. The area is relatively unknown geologically and is believed to lie in the middle of the Palaeozoic Daly Basin, overlain by shallow Cretaceous sediments, and younger surficial deposits. Only surficial deposits are mapped in the area. . During the initial phase of exploration of EL23684, work consisted of literature research of previous exploration, geological survey and geophysical survey over the EL and surrounding district. It also included data compilation, acquisition and interpretation of departmental geological and airborne geophysical data sets. In addition, visits to other stakeholders in the area for introduction purposes were completed, and the Sacred Sites register was searched. In year 2, a visit to the area was made in company with the Company's diamond expert consultant to inspect possible sample sites identified from studies of imagery and airborne geophysics. It was decided that it would be necessary to do shallow drilling of drainage channels to collect suitable material for heavy mineral analysis. Additional rock chip samples were collected and these returned anomalous metal values consistent with those previously obtained. The results of rock samples are broadly anomalous for a range of metals associated with a wide range of mineralisation types. Further work is warranted to characterise the target and locate a centre to the widespread elevated values.
Date Added: 23-Oct-2013
Appears in Collections:Minerals Exploration Reports (MEX)

Files in this Report:
File SizeFormat Add to
Download
EL23684_2006_A_01.pdf1.65 MBPDF Add
EL23684_2006_A_02_Geochemical_Result.xls25 kBMicrosoft Excel Add


Items in GEMIS are protected by copyright unless otherwise indicated.

Get Adobe Reader