Browsing by Author "Taran M.N."
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Browsing by Author "Taran M.N."
Now showing items 1-13 of 13
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Richter H.; Posch T.; Taran M.N.; Mutschke H. (2005)Among the oxides, spinels are relatively abundant constituents of stardust, as has been inferred from studies of presolar grains in meteorites. Up to now, only pure Mg-Al-spinels have been considered as a possible stardust ...
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Taran M.N.; Langer K. (2001)Polarized electronic single crystal spectra of natural Fe2+ ion-bearing oxygen-based minerals, in which ferrous ions enter octahedral sites of different symmetry and distortion (olivine, cordierite, ortho- and clinopyroxene, ...
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Taran M.N.; Langer K. (2000)Temperature, T, and pressure, P, behaviour of absorption bands caused by spin-forbidden dd-transitions of Fe3+ in octahedral sites of the andradite and epidote structures were studied at T from 300 to 750 K and P up to 10 ...
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Platonov A.N.; Taran M.N.; Langer K.; Chopin C.; Andrut M. (2000)Single crystals of several varieties of dumortierite, an orthorhombic, pseudohexagonal borosilicate mineral with spectacular colour and pleochroism, were studied by electronic absorption spectroscopy and electron-microprobe ...
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Taran M.N.; Rossman G.R. (2002)The optical spectra of dravite (tourmaline) with an unusually high ratio of Fe3+ to Fe2+ and a synthetic elbaite with high Fe3+ content were studied at high temperature (297 to 600 K) and high pressure (to 10.51 GPa) ...
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Taran M.N.; Platonov A.N.; Langer K.; Abs-Wurmbach I.; Frost D.J. (2004)Pyrope-knorringite garnets, Mg3(Al1-X Cr3+X)2Si3O12 with X=0.25, 0.50, and 1.00, were synthesized between 9 and 16 GPa and 1300 and 1600 °C, using multianvil high-pressure techniques. The garnets with X=0.25 and 0.50 are ...
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Taran M.N.; Silayev V.I.; Khomenko V.N.; Ivanova I.B.; Zharikov V.A. (1989)A lilac- to violet-colored mineral subsequently identified as rhodonite was found by I.B. Ivanova in a carbonate-manganese ores of the Polar Urals in 1985. The manganese show consisted of a lens within Riphaean ...
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Taran M.N.; Kvasnytsya V.M.; Langer K. (2004)A distinctive feature of Ukrainian deep-violet diamond microcrystals is a broad absorption band centered at about 560 nm (17850cm(-1) or 2.21 eV). In the Ukrainian samples, the intensity of this band is almost two orders ...
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Taran M.N.; Rossman G.R. (2001)Polarized optical absorption spectra of three synthetic Co-bearing silicates, orthopyroxene, olivine and beryl, were studied at room and liquid nitrogen temperatures. In all three matrices, Co enters octahedral structural ...
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Taran M.N.; Rossman G.R. (2001)Polarized optical absorption spectra of a rare Fe2+, Fe3+-bearing silicate mineral, tuhualite, (Na,K)2Fe22+Fe23+Si12O30, were measured at room temperature in the range 350–4000 nm (ca. 28500–2500 cm–1). The spectra display ...
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Taran M.N.; Langer K.; Geiger C.A. (2002)Single crystals of synthetic vanadium-, chromium- and cobalt-bearing garnets, Pyr:V0.06, Pyr:V0.13, Pyr:Cr0.04, Pyr:Co0.10, and Gt:Co3.00, and a natural vanadium-bearing grossular, Gross:V0.07 (Cr3+ < 0.005), were studied ...
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Taran M.N.; Langer K. (2003)Unpolarized, (X,Y)-mixed electronic absorption spectra were measured on (001) plates of two natural orthopyroxenes with 24 and 45 mole % ferrosilite and with a Ca content 0.07 atoms pfu, at pressures up to 10.3 and 8.83 ...
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Rossman G.R.; Taran M.N. (2001)Optical spectra are presented for seven oxygen based, four-coordinated Fe2+ bearing minerals, eudialyte, gehlenite, genthelvite, gillespite, pellyite, spinel, and staurolite, and two five-coordinated Fe2+ minerals, ...
Now showing items 1-13 of 13