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1 Institute of Geochemistry, Mineralogy and Ore Formation, National Academy of Science of Ukraine, Palladin Avenue, 34, 03680 Kyiv-142, Ukraine
2 Deutsches GeoForschungsZentrum, Sektion 3.3, Telegrafenberg, 14473 Potsdam, Germany
Correspondence: * E-mail: m_taran{at}hotmail.com
Optical absorption spectra of natural Co-bearing spinel and staurolite were studied at different temperatures and pressures. In both minerals, two broad, intense structured bands in the range 5500–8000 and 15 000–19 000 cm–1, caused by electronic spin-allowed transitions 4A2
4T1(4F) and 4A2
4T1(4P) of IVCo2+ are the predominant absorption features. In addition, in both cases broad bands, derived from spin-allowed electronic transitions 4E
4T2 of IVFe2+, appear in the near infrared range partly overlapping the bands caused by IVCo2+. In staurolite the NIR range of the spectra are complicated by intense sharp lines of OH-vibrations at around 3400 cm–1.
In spinel, with a regular tetrahedral site, the splitting of the spin-allowed bands I and II of IVCo2+ is assumed to be caused by spin-orbit and vibronic coupling. In staurolite, the splitting is stronger due to the additional low-symmetry crystal field effect of IVCo2+. It is found that the effect of temperature and pressure on the behavior of the 4A2
4T1(4P) bands of IVCo2+ in the two minerals are rather similar, in contrast to our findings for the spin-allowed bands of IVFe2+ in spinel and staurolite. This is interpreted as a manifestation of a dynamic Jahn-Teller effect for IVFe2+ and lack of it in case of IVCo2+.
Key Words: Spinel staurolite tetrahedral coordination Co2+ optical absorption spectra temperature and pressure effects
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