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Distribution and Substitution Mechanism of Ge in a Ge-(Fe)-Bearing Sphalerite

DOI: 10.3390/min5020117 DOI Help

Authors: Nigel Cook (University of Adelaide) , Barbara Etschmann (University of Adelaide) , Cristiana Ciobanu-cook (University of Adelaide) , Tina Geraki (Diamond Light Source) , Daryl Howard (Australian Synchrotron) , Timothy Williams (Monash University) , Nick Rae (Monash University) , Allan Pring (South Australian Museum) , Guorong Chen (East China University of Science and Technology) , Bernt Johannessen (Australian Synchrotron) , Joel Brugger (Monash University)
Co-authored by industrial partner: No

Type: Journal Paper
Journal: Minerals , VOL 5 (2) , PAGES 117 - 132

State: Published (Approved)
Published: March 2015
Diamond Proposal Number(s): 7563

Open Access Open Access

Abstract: The distribution and substitution mechanism of Ge in the Ge-rich sphalerite from the Tres Marias Zn deposit, Mexico, was studied using a combination of techniques at micro m- to atomic scales. Trace element mapping by Laser Ablation Inductively Coupled Mass Spectrometry shows that Ge is enriched in the same bands as Fe, and that Ge-rich sphalerite also contains measurable levels of several other minor elements, including As, Pb and Tl. Micron- to nanoscale heterogeneity in the sample, both textural and compositional, is revealed by investigation using Focused Ion Beam-Scanning Electron Microscopy (FIB-SEM) combined with Synchrotron X-ray Fluorescence mapping and High-Resolution Transmission Electron Microscopy imaging of FIB-prepared samples. Results show that Ge is preferentially incorporated within Fe-rich sphalerite with textural complexity finer than that of the microbeam used for the X-ray Absorption Near Edge Structure (XANES) measurements. Such heterogeneity, expressed as intergrowths between 3C sphalerite and 2H wurtzite on [11¯0] zones, could be the result of either a primary growth process, or alternatively, polystage crystallization, in which early Fe-Ge-rich sphalerite is partially replaced by Fe-Ge-poor wurtzite. FIB-SEM imaging shows evidence for replacement supporting the latter. Transformation of sphalerite into wurtzite is promoted by (111)* twinning or lattice-scale defects, leading to a heterogeneous ZnS sample, in which the dominant component, sphalerite, can host up to ~20% wurtzite. Ge K-edge XANES spectra for this sphalerite are identical to those of the germanite and argyrodite standards and the synthetic chalcogenide glasses GeS2 and GeSe2, indicating the Ge formally exists in the tetravalent form in this sphalerite. Fe K-edge XANES spectra for the same sample indicate that Fe is present mainly as Fe2+, and Cu K-edge XANES spectra are characteristic for Cu+. Since there is no evidence for coupled substitution involving a monovalent element, we propose that Ge4+ substitutes for (Zn2+, Fe2+) with vacancies in the structure to compensate for charge balance. This study shows the utility of synchrotron radiation combined with electron beam micro-analysis in investigating low-level concentrations of minor metals in common sulfides.

Subject Areas: Earth Science

Instruments: B18-Core EXAFS , I18-Microfocus Spectroscopy

Other Facilities: Australian Synchrotron