Abstract
The new mineral graţianite, MnBi2S4, is described from the Bǎiţa Bihor skarn deposit, Bihor County, Romania. Graţianite occurs as thin lamellae, intimately intergrown with cosalite and bismuthinite, or as flower-shaped blebs within chalcopyrite, where it is associated with cosalite and tetradymite. Graţianite displays weak to modest bireflectance in air and oil, respectively, and strong anisotropy. The mean empirical composition based on 20 electron probe microanalyses is: (Mn0.541Fe0.319Pb0.070Cu0.040 Cd0.009 Ag0.001)S0.980(Bi1.975Sb0.018)S1.993(S4.008Se0.012Te0.007)S4.027, corresponding to the ideal formula MnBi2S4. Graţianite crystallizes in the monoclinic system (space group C2/m). Single-crystal X-ray studies of material extracted by the focused ion beam-scanning electron microscopy (FIB-SEM) technique, and carried out on the MX2 macromolecular beamline of the Australian Synchrotron determined the following cell dimensions: a = 12.6774(25) Å, b = 3.9140(8) Å, c = 14.7581(30) Å, b = 115.31(3)°, V = 662.0(2) Å3, and Z = 4. The six strongest X-ray reflections and their relative intensities are: 3.448 Å (100), 2.731 Å (77), 2.855 Å (64), 3.637 Å (55), 3.644 Å (54), and 3.062 Å (51).
Graţianite is the monoclinic analog of berthierite (FeSb2S4), garavellite [Fe(Bi,Sb)2S4] and clerite [Mn(Sb,As)2S4] (Nickel-Strunz class 02.HA.20). It is isostructural with synthetic sulfides and selenides in the MnBi2S4-MnSb2S4 and MnBi2Se4-MnSb2Se4 series, and with grumiplucite (HgBi2S4) and kudriavite, [(Cd,Pb)Bi2S4], 3P members of the pavonite homologous series. The mineral is named for Graţian Cioflica (1927-2002), formerly Professor in Mineralogy and Ore Deposits at the University of Bucharest, Romania. The Băiţa Bihor skarn, like others within the same belt, is geochemically complex. The availability of Cu, Zn, and Pb, but also Ag, Bi, Mo, and B, as well as a wide range of minor elements, has created an environment allowing for crystallization of an unusually diverse range of discrete minerals. Graţianite is part of the peculiar associations of Bi-Pb-sulfosalts and Bi-chalcogenides that are genetically related to Au-enrichment. This study demonstrates the versatility of FIB-SEM techniques for in situ extraction of small volumes of well-characterized material, coupled with single-crystal X-ray analysis using synchrotron radiation, for the characterization of new minerals
© 2014 by Walter de Gruyter Berlin/Boston
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- Dolomite discloses a hidden history of subducting slabs
- Crossroads in Earth and Planetary Materials
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- High-pressure behavior of thiospinel CuCr2S4
- Martian Rocks and Soil
- Mössbauer parameters of iron in phosphate minerals: Implications for interpretation of martian data
- A temperature-controlled sample stage for in situ micro-X-ray diffraction: Application to Mars analog mirabilite-bearing perennial cold spring precipitate mineralogy
- Detection of iron substitution in natroalunite-natrojarosite solid solutions and potential implications for Mars
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- An assessment of the reliability of melt inclusions as recorders of the pre-eruptive volatile content of magmas
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- Ophirite, Ca2Mg4[Zn2Mn23+(H2O)2(Fe3+W9O34)2]·46H2O, a new mineral with a heteropolytungstate tri-lacunary Keggin anion
- Bubble formation during decompression of andesitic melts
- Manganese carbonate formation from amorphous and nanocrystalline precursors: Thermodynamics and geochemical relevance
- Insights into the crystal chemistry of Earth materials rendered by electron density distributions: Pauling’s rules revisited
- Adsorption of sulfur dioxide on volcanic ashes
- Sulfidation of native gold
- Electrical conductivity of synthetic mullite single crystals
- In situ Raman spectroscopy identification of the S3̅ ion in S-rich hydrothermal fluids from synthetic fluid inclusions
- Melting phase equilibria of model carbonated peridotite from 8 to 12 GPa in the system CaO-MgO-Al2O3-SiO2-CO2 and kimberlitic liquids in the Earth’s upper mantle
- Effect of orientation on ion track formation in apatite and zircon
- Major, minor, and trace element composition of pyromorphite-group minerals as recorder of supergene weathering processes from the Schwarzwald mining district, SW Germany
- Toward an accurate ab initio estimation of compressibility and thermal expansion of diamond in the [0, 3000 K] temperature and [0, 30 GPa] pressures ranges, at the hybrid HF/DFT theoretical level
- Vanadio-oxy-chromium-dravite, NaV3(Cr4Mg2)(Si6O18)(BO3)3(OH)3O, a new mineral species of the tourmaline supergroup
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- Valence state partitioning of V between pyroxene and melt for martian melt compositions Y 980459 and QUE 94201: The effect of pyroxene composition and crystal structure
- MSA Award Presentations
- Presentation of the Mineralogical Society of America Award for 2013 to Wendy Li-Wen Mao
- Acceptance of the Mineralogical Society of America Award for 2013
- Presentation of the 2013 Roebling Medal of the Mineralogical Society of America to Frank C. Hawthorne
- Acceptance of the 2013 Roebling Medal of the Mineralogical Society of America
- Presentation of the Distinguished Public Service Award for 2013 of the Mineralogical Society of America to Pierrette Tremblay
- Acceptance of the Distinguished Public Service Award for 2013 of the Mineralogical Society of America
- Presentation of the Dana Medal of the Mineralogical Society of America for 2014 to Patricia Dove
- Acceptance of the Dana Medal of the Mineralogical Society of America for 2014
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