A Comparison of In Situ Analytical Methods for Trace Element Measurement in Gold Samples from Various South African Gold Deposits

被引:11
作者
Gauert, Christoph [1 ]
Schannor, Mathias [2 ,3 ]
Hecht, Lutz [3 ]
Radtke, Martin [4 ]
Reinholz, Uwe [4 ]
机构
[1] Univ Free State, Dept Geol, ZA-9300 Bloemfontein, South Africa
[2] Free Univ Berlin, Inst Geol Wissensch, D-12249 Berlin, Germany
[3] Leibniz Inst Evolut & Biodiversitatsforsch, Museum Nat Kunde, D-10115 Berlin, Germany
[4] BAM Fed Inst Mat Res & Testing, D-12489 Berlin, Germany
基金
新加坡国家研究基金会;
关键词
trace elements; gold; FE-EPMA; LA-ICP-MS; SR-mu-XRF; precision; PLASMA-MASS SPECTROMETRY; HIGH-ENERGY; ICP-MS; WITWATERSRAND; FEMTOSECOND; PLACER; GRAINS; MERCURY; SILVER; XRF;
D O I
10.1111/j.1751-908X.2015.00362.x
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Trace element concentrations in gold grains from various geological units in South Africa were measured in situ by field emission-electron probe microanalysis (FE-EPMA), laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) and synchrotron micro X-ray fluorescence spectroscopy (SR-mu-XRF). This study assesses the accuracy, precision and detection limits of these mostly non-destructive analytical methods using certified reference materials and discusses their application in natural sample measurement. FE-EPMA point analyses yielded reproducible and discernible concentrations for Au and trace concentrations of S, Cu, Ti, Hg, Fe and Ni, with detection limits well below the actual concentrations in the gold. LA-ICP-MS analyses required larger gold particles (> 60 mu m) to avoid contamination during measurement. Elements that measured above detection limits included Ag, Cu, Ti, Fe, Pt, Pd, Mn, Cr, Ni, Sn, Hg, Pb, As and Te, which can be used for geochemical characterisation and gold fingerprinting. Although LA-ICP-MS measurements had lower detection limits, precision was lower than FE-EPMA and SR-mu-XRF. The higher variability in absolute values measured by LA-ICP-MS, possibly due to micro-inclusions, had to be critically assessed. Non-destructive point analyses of gold alloys by SR-l-XRF revealed Ag, Fe, Cu, Ni, Pb, Ti, Sb, U, Cr, Co, As, Y and Zr in the various gold samples. Detection limits were mostly lower than those for elements measured by FE-EPMA, but higher than those for elements measured by LA-ICP-MS.
引用
收藏
页码:267 / 289
页数:23
相关论文
共 48 条
[1]   Trace-element and U-Pb isotope compositions of pyrite types in the Proterozoic Black Reef, Transvaal Sequence, South Africa: Implications on genesis and age [J].
Barton, ES ;
Hallbauer, DK .
CHEMICAL GEOLOGY, 1996, 133 (1-4) :173-199
[2]   Trace element fingerprinting of ancient Chinese gold with femtosecond laser ablation-inductively coupled mass spectrometry [J].
Brostoff, Lynn B. ;
Gonzalez, Jhanis J. ;
Jett, Paul ;
Russo, Richard E. .
JOURNAL OF ARCHAEOLOGICAL SCIENCE, 2009, 36 (02) :461-466
[3]  
Chao A. W., 2013, Handbook of Accelerator Physics and Engineering
[4]   Microchemical characterization of alluvial gold grains as an exploration tool [J].
Chapman, R ;
Leake, B ;
Styles, M .
GOLD BULLETIN, 2002, 35 (02) :53-65
[5]  
Dixon R. D., 2013, 6 IGN MET STUD GROUP, P20
[6]  
Donovan JJ., 1993, MICROBEAM ANAL, V2, P23, DOI DOI 10.1017/S0424820100132868
[7]  
Fialin M, 1999, AM MINERAL, V84, P70
[8]  
Foya S. N., 2001, THESIS
[9]   Milli-PIXE of coexisting cooperite and braggite - a comparison with electron probe microanalysis [J].
Franklyn, CB ;
Merkle, RKW .
NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS, 1999, 158 (1-4) :550-555
[10]  
Frimmel H.E., 2002, SPECIAL PUBLICATION, P221