Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/120611
Citations
Scopus Web of Science® Altmetric
?
?
Type: Journal article
Title: Detection of trace elements/isotopes in Olympic Dam copper concentrates by nanoSIMS
Author: Rollog, M.
Cook, N.J.
Guagliardo, P.
Ehrig, K.
Ciobanu, C.L.
Kilburn, M.
Citation: Minerals, 2019; 9(6):1-25
Publisher: MDPI AG
Issue Date: 2019
ISSN: 2075-163X
2075-163X
Statement of
Responsibility: 
Mark Rollog, Nigel J. Cook, Paul Guagliardo, Kathy Ehrig, Cristiana L. Ciobanu and Matt Kilburn
Abstract: Many analytical techniques for trace element analysis are available to the geochemist and geometallurgist to understand and, ideally, quantify the distribution of trace and minor components in a mineral deposit. Bulk trace element data are useful, but do not provide information regarding specific host minerals—or lack thereof, in cases of surface adherence or fracture fill—for each element. The CAMECA nanoscale secondary ion mass spectrometer (nanoSIMS) 50 and 50L instruments feature ultra-low minimum detection limits (to parts-per-billion) and sub-micron spatial resolution, a combination not found in any other analytical platform. Using ore and copper concentrate samples from the Olympic Dam mining-processing operation, South Australia, we demonstrate the application of nanoSIMS to understand the mineralogical distribution of potential by-product and detrimental elements. Results show previously undetected mineral host assemblages and elemental associations, providing geochemists with insight into mineral formation and elemental remobilization—and metallurgists with critical information necessary for optimizing ore processing techniques. Gold and Te may be seen associated with brannerite, and Ag prefers chalcocite over bornite. Rare earth elements may be found in trace quantities in fluorapatite and fluorite, which may report to final concentrates as entrained liberated or gangue-sulfide composite particles. Selenium, As, and Te reside in sulfides, commonly in association with Pb, Bi, Ag, and Au. Radionuclide daughters of the 238U decay chain may be located using nanoSIMS, providing critical information on these trace components that is unavailable using other microanalytical techniques. These radionuclides are observed in many minerals but seem particularly enriched in uranium minerals, some phosphates and sulfates, and within high surface area minerals. The nanoSIMS has proven a valuable tool in determining the spatial distribution of trace elements and isotopes in fine-grained copper ore, providing researchers with crucial evidence needed to answer questions of ore formation, ore alteration, and ore processing.
Keywords: Radionuclides; trace elements; isotopes; nanoSIMS; copper concentrate; Olympic Dam
Rights: © 2019 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).
RMID: 0030120812
DOI: 10.3390/min9060336
Grant ID: http://purl.org/au-research/grants/arc/IH130200033
Appears in Collections:Chemical Engineering publications

Files in This Item:
File Description SizeFormat 
hdl_120611.pdfPublished version9.14 MBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.