Data

Spectra and images from single-crystal Ramen Spectroscopy of natural schafarzikite FeSb2O4 from Pernek, Slovak Republic

Queensland University of Technology
Bahfenne, Silmarilly ; Rintoul, Llew ; Frost, Ray
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.4225/09/58859ca66c488&rft.title=Spectra and images from single-crystal Ramen Spectroscopy of natural schafarzikite FeSb2O4 from Pernek, Slovak Republic&rft.identifier=10.4225/09/58859ca66c488&rft.publisher=Queensland University of Technology&rft.description=As part of a larger study of arsenite and antimonite minerals, we report the single-crystal Raman spectrum of natural schafarzikite FeSb2O4 and the non-oriented Raman spectra of its Zn analog and the related minerals, apuanite and trippkeite. Figure 1 shows XRD patterns of the products formed in (a) ZnSb2O4 and (b) CuAs2O4 syntheses.  Figure 2 is SEM images of (a) natural schafarzikite, (b) synthetic ZnSb2O4, and (c) synthetic trippkeite.  Figure 3 is Peak-fitted Raman spectrum of schafarzikite in the 900–100 cm−1region.  Figure 4 shows (a) Oriented single-crystal Raman spectrum of schafarzikite in the 400–100 cm−1 region. (b) Oriented single-crystal Raman spectrum of schafarzikite in the 900–300 cm−1region. Figure 5 is Peak-fitted Raman spectrum of ZnSb2O4 in the 800–100 cm−1region. &rft.creator=Bahfenne, Silmarilly &rft.creator=Rintoul, Llew &rft.creator=Frost, Ray &rft.date=2015&rft.edition=1&rft.coverage=150.396206,-23.339753 150.516712,-23.339753 150.516712,-23.416962 150.396206,-23.416962 150.396206,-23.339753&rft_rights=? American Mineralogist, 2011&rft_subject=trippkeite&rft_subject=Schafarzikite&rft_subject=single-crystal Ramon spectroscopy&rft_subject=antimonite&rft_subject=apuanite&rft.type=dataset&rft.language=English Access the data

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Postal Address:
Emeritus Professor Ray Frost

r.frost@qut.edu.au

Full description

As part of a larger study of arsenite and antimonite minerals, we report the single-crystal Raman spectrum of natural schafarzikite FeSb2O4 and the non-oriented Raman spectra of its Zn analog and the related minerals, apuanite and trippkeite.

Figure 1 shows XRD patterns of the products formed in (a) ZnSb2O4 and (b) CuAs2O4 syntheses.  Figure 2 is SEM images of (a) natural schafarzikite, (b) synthetic ZnSb2O4, and (c) synthetic trippkeite.  Figure 3 is Peak-fitted Raman spectrum of schafarzikite in the 900–100 cm−1region.  Figure 4 shows (a) Oriented single-crystal Raman spectrum of schafarzikite in the 400–100 cm−1 region. (b) Oriented single-crystal Raman spectrum of schafarzikite in the 900–300 cm−1region. Figure 5 is Peak-fitted Raman spectrum of ZnSb2O4 in the 800–100 cm−1region.

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150.39621,-23.33975 150.51671,-23.33975 150.51671,-23.41696 150.39621,-23.41696 150.39621,-23.33975

150.456459,-23.3783575

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