Please use this identifier to cite or link to this item:
Export to Endnote
https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/80110
Export to Endnote
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Humphries, B | en_US |
dc.date.accessioned | 2015-06-26T04:32:59Z | - |
dc.date.issued | 2014 | en_US |
dc.identifier.govdoc | CR2014-0365 | en_US |
dc.identifier.uri | https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/80110 | en_US |
dc.description.abstract | During this reporting period Krucible has completed a sampling program over identified areas within the EL. These areas were subject to lag surface geochemical sampling and rock chip-grab sampling. Results of the lag returned anomalous base metal results including a corridor of anomalous lead in the Elstone prospect. Assayed of up to 228ppm copper, 264ppm lead, and 269ppm zinc were recorded. Other anomalous elements include up to 0.54ppm silver and 0.1ppm gold. These results are considered very encouraging for mineralisation. | en_US |
dc.subject.classification | Iron oxides | en_US |
dc.subject.classification | Base metals | en_US |
dc.subject.classification | Copper | en_US |
dc.subject.classification | Lead | en_US |
dc.subject.classification | Zinc | en_US |
dc.subject.classification | Precious metals | en_US |
dc.subject.classification | Gold | en_US |
dc.subject.classification | Regional geology | en_US |
dc.subject.classification | Cambrian | en_US |
dc.subject.classification | Proterozoic | en_US |
dc.subject.classification | Structure | en_US |
dc.subject.classification | Exploration philosophy | en_US |
dc.subject.classification | Exploration history | en_US |
dc.subject.classification | Geological mapping | en_US |
dc.subject.classification | Geophysical interpretation | en_US |
dc.subject.classification | Geochemical anomalies | en_US |
dc.subject.classification | Geochemical exploration | en_US |
dc.subject.classification | Geochemical sampling | en_US |
dc.subject.classification | Lag sampling | en_US |
dc.subject.classification | Grab sampling | en_US |
dc.subject.classification | Rock chip sampling | en_US |
dc.subject.classification | Assaying | en_US |
dc.subject.classification | Assay value | en_US |
dc.title | EL 28170 Tobermorey Annual report for period ending 3 April 2014 | en_US |
dc.relation.isatmap100 | Adam 6451 | en_US |
dc.relation.isatmap100 | Field River 6450 | en_US |
dc.relation.isatmap250 | Hay River SF5316 | en_US |
dc.relation.isatgeolprovince | Georgina Basin | en_US |
dc.description.stratname | Arunta Complex, Strangways Metamorphic Complex | en_US |
dc.description.geochemicalsampling | 22 Rock chip samples | en_US |
dc.description.geochemicalsampling | 132 Lag samples | en_US |
dc.description.mineprospectname | Elstone | en_US |
dc.identifier.tenure | EL28170 | en_US |
dc.description.modifyhistory | 14/07/2014 | en_US |
dc.description.modifyhistory | 19/06/2015 | en_US |
dc.description.modifyhistory | 19/09/2017 | en_US |
dc.contributor.holder | Krucible Metals | en_US |
dc.identifier.collectionname | Minerals Exploration Reports (MEX) | en_US |
dc.identifier.govdocprefix | CR2014 | en_US |
local.flag.notified | 1 | |
Appears in Collections: | Minerals Exploration Reports (MEX) |
Files in this Report:
File | Size | Format | Add to Download |
---|---|---|---|
EL28170_2014_A_01.pdf | 594.15 kB | Add | |
EL28170_2014_A_02_FIGURE1.pdf | 298.19 kB | Add | |
EL28170_2014_A_03_FIGURE2.pdf | 475.6 kB | Add | |
EL28170_2014_A_04_FIGURE3.pdf | 278.66 kB | Add | |
EL28170_2014_A_05_FIGURE4.pdf | 368.88 kB | Add | |
EL28170_2014_A_06_FIGURE5.pdf | 257.75 kB | Add | |
EL28170_2014_A_07_FIGURE6.pdf | 238.01 kB | Add | |
EL28170_2014_A_08_FIGURE7.pdf | 380.19 kB | Add | |
EL28170_2014_A_09_FIGURE8.pdf | 407.99 kB | Add | |
EL28170_2014_A_10_RockChips.txt | 12.48 kB | Text | Add |
EL28170_2014_A_11_RockChipsCodes.txt | 516 B | Text | Add |
EL28170_2014_A_12_SurfaceGeochem.txt | 44.34 kB | Text | Add |
EL28170_2014_A_13_SurfaceGeochemCodes.txt | 194 B | Text | Add |
Items in GEMIS are protected by copyright unless otherwise indicated.