Please use this identifier to cite or link to this item:
Export to Endnote
https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/86862
Export to Endnote
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | McGloin, MV | en_US |
dc.contributor.author | Matchan, E | en_US |
dc.contributor.author | Phillips, D | en_US |
dc.date.accessioned | 2018-01-04T01:32:52Z | - |
dc.date.issued | 2018 | en_US |
dc.identifier.govdoc | NTGS Record 2017-013 | en_US |
dc.identifier.isbn | 9780724573240 (PDF) | en_US |
dc.identifier.issn | 1443-1149 | en_US |
dc.identifier.uri | https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/86862 | en_US |
dc.description.abstract | This Record details 40Ar/39Ar step-heating analysis of hornblende sampled from the polymetallic Cu-Pb (Zn-Ag-Au) Johnnies Reward prospect, ALICE SPRINGS, in Aileron Province, central Australia. A sample of hornblende (AS15MVM034) was collected from an outcropping quartz vein associated with pegmatite intrusions that cross-cut the Cadney Metamorphics and mineralisation at the prospect. Hornblende was dated to determine the timing of vein formation and any potential overprinting episodes of fluid-flow and/or metamorphism. If the quartz vein is pegmatite-related, any age yielded may date pegmatite emplacement. Because the sampled quartz vein cross-cuts the mineralised host assemblage, dating of the hornblende will also constrain a minimum age for mineralisation at the prospect. | en_US |
dc.description.abstract | Hornblende from sample AS15MVM034 produced a discordant age spectrum of anomalously old apparent ages of ca 3.8 -1.6 Ga for the low-temperature steps (steps 1-3), decreasing to ca 900-800 Ma (steps 4-5), and then to ~650 -600 Ma for the remaining 55% of the gas release profile (steps 6-12). Inverse isochron ages for the same sample (making no assumption about initial 40Ar/36Ar sample values) produced concordant data for the mid- to high-temperature (steps 6 to 12), and revealed the presence of excess argon in the sample. This indicates that age spectrum ages (which are calculated assuming an atmospheric initial 40Ar/36Ar ratio) are verestimated. The inverse isochron age generated through steps 6 to 12 is 428 ± 31 Ma (2s; MSWD = 1.6, probability of fit = 0.16). This age is consistent with the timing of the ca 450-300 Ma Alice Springs Orogeny and provides a minimum age constraint for mineralisation at Johnnies Reward. | en_US |
dc.publisher | Northern Territory Geological Survey | en_US |
dc.rights.uri | <a href="https://creativecommons.org/licenses/by/4.0/" target="_blank">Creative Commons Attribution 4.0 International</a> (CC BY 4.0). Please observe and retain any copyright or related notices that accompany this material and give attribution to: Northern Territory of Australia (Northern Territory Geological Survey). | en_US |
dc.subject.classification | Geochronology | en_US |
dc.title | Summary of results. 40Ar/39Ar step-heating hornblende dating, Johnnies Reward prospect, Strangways Range, Aileron Province | en_US |
dc.type | NTGS Record | en_US |
dc.relation.isatmap250 | Alice Springs SF5314 | en_US |
dc.relation.isatgeolprovince | Aileron Province | en_US |
dc.relation.isatgeolprovince | Arunta Region | en_US |
dc.description.mineprospectname | Johnnies Reward | en_US |
dc.identifier.collectionname | Reports, Records, Books | |
dc.identifier.govdocprefix | NTGS Record 2017 | en_US |
local.flag.notified | 1 | |
Appears in Collections: | Reports, Records, Books |
Files in this Report:
File | Size | Format | Add to Download |
---|---|---|---|
NTGSRec2017-013.zip | 6.3 MB | ZIP | Add |
Items in GEMIS are protected by copyright unless otherwise indicated.