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Data Publication

Quantitative mineralogy, mineral chemistry and microtex-tural data on the UG2 chromitite intruded by iron-rich ul-tramafic pegmatite (IRUP) at the Thaba Mine, northwest-ern Bushveld Complex, South Africa

Zhou, Haoyang | Appelt, Oona | Tjallingii, Rik | Bachmann, Kai | Trumbull, Robert B.

GFZ Data Services

(2023)

Discordant iron-rich ultramafic pegmatites (IRUPs) intersect the UG2 chromitite at many places in the Bushveld Complex but the effects on ore grade and mineralogy have rarely been studied in detail. We investigated a drillcore profile through the UG2 layer affected by IRUP intrusions at Tha-ba mine, NW Bushveld. The work involved quantitative assessment of the ore mineralogy from mineral liberation analysis (MLA), chemical analyses of the main silicate and oxide minerals by elec-tron microprobe (EPMA) and micro-X-ray fluorescence (micro-XRF) element maps of the UG2-IRUP contacts. The data reveal features of UG2-IRUP interaction at different scales. The micro-XRF study of the contacts shows that a thin layer of Fe-Ti-Cr spinel and ilmenite formed on the IRUP side, while chromite on the UG2 side underwent grain coarsening with loss of interstitial space, and developed chemical gradients in Cr, Al, Fe and Ti. On a larger scale, the MLA data document changes in ore and gangue mineral assemblages through most of the meter-thick UG2 layer. This includes formation of secondary hydrous silicates, replacement of PGE- sulfides by PGE alloys and PGE- As-Sb-Bi-Te-Pb phases, and formation of secondary Ni-Cu-Fe sulfides after pentlandite and chalcopyrite.

Keywords


MSL enriched keywords
igneous rock - intrusive
acidic intrusive
pegmatite
minerals
chemical elements
iron
measured property
iron
Analyzed feature
mineralogy and composition
quantitative mineralogy
sulfide minerals
chalcopyrite
pentlandite
oxide mineral
chromite
ilmenite
spinel
equipment
electron probe micro-analyzer
x-ray spectrometer
x-ray fluorescence spectrometer
aluminium
chromium
Apparatus
microchemical analysis
electron probe micro analyser
Equipment
borehole drilling
drill core

MSL enriched sub domains i

geochemistry
microscopy and tomography
geo-energy test beds


Source publisher

GFZ Data Services


DOI

10.5880/gfz.3.1.2022.005


Authors

Zhou, Haoyang

0000-0002-0079-503X

Natural History Museum, University of Oslo, Oslo, Norway; GFZ German Research Centre for Geosciences, Potsdam, Germany;

Appelt, Oona

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Tjallingii, Rik

0000-0002-9723-3622

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Bachmann, Kai

Helmholtz-Centre Dresden-Rossendorf, Helmholtz Institute Freiberg of Resource Technology, Freiberg, Germany;

Trumbull, Robert B.

0000-0002-1999-4653

GFZ German Research Centre for Geosciences, Potsdam, Germany;


Contributers

Microprobe Lab (GFZ German Research Centre for Geosciences, Germany)

HostingInstitution

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Laboratory for XRF Element Scanning ((GFZ German Research Centre for Geosciences, Germany)

HostingInstitution

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Trumbull, Robert B.

ContactPerson

GFZ German Research Centre for Geosciences, Potsdam, Germany;


References

Zhou, H., Trumbull, R. B., Veksler, I. V., & Bachmann, K. (2023). The effects of iron-rich ultramafic pegmatite on the composition and mineralogy of the UG2 chromitite: a case study in the western Bushveld Complex, South Africa. Mineralium Deposita, 58(6), 1005–1021. https://doi.org/10.1007/s00126-023-01167-x

10.1007/s00126-023-01167-x

IsSupplementTo

Bachmann, K., Frenzel, M., Krause, J., & Gutzmer, J. (2017). Advanced Identification and Quantification of In-Bearing Minerals by Scanning Electron Microscope-Based Image Analysis. Microscopy and Microanalysis, 23(3), 527–537. https://doi.org/10.1017/s1431927617000460

10.1017/S1431927617000460

Cites

Bachmann, K., Osbahr, I., Tolosana-Delgado, R., Chetty, D., & Gutzmer, J. (2018). Variation in Platinum Group Mineral and Base Metal Sulfide Assemblages in the Lower Group Chromitites of the Western Bushveld Complex, South Africa. The Canadian Mineralogist, 56(5), 723–743. https://doi.org/10.3749/canmin.1700094

10.3749/canmin.1700094

Cites

Fandrich, R., Gu, Y., Burrows, D., & Moeller, K. (2007). Modern SEM-based mineral liberation analysis. International Journal of Mineral Processing, 84(1–4), 310–320. https://doi.org/10.1016/j.minpro.2006.07.018

10.1016/j.minpro.2006.07.018

Cites

Ferracutti, G. R., Gargiulo, M. F., Ganuza, M. L., Bjerg, E. A., & Castro, S. M. (2014). Determination of the spinel group end-members based on electron microprobe analyses. Mineralogy and Petrology, 109(2), 153–160. https://doi.org/10.1007/s00710-014-0363-1

10.1007/s00710-014-0363-1

Cites


Contact

Trumbull, Robert B.

GFZ German Research Centre for Geosciences, Potsdam, Germany;


Citiation

Zhou, H., Appelt, O., Tjallingii, R., Bachmann, K., & Trumbull, R. B. (2023). Quantitative mineralogy, mineral chemistry and microtex-tural data on the UG2 chromitite intruded by iron-rich ul-tramafic pegmatite (IRUP) at the Thaba Mine, northwest-ern Bushveld Complex, South Africa [Data set]. GFZ Data Services. https://doi.org/10.5880/GFZ.3.1.2022.005


Geo location(s)

Thaba Mine, northwestern Bushveld Complex, South Africa