Abstract
Oxy-dravite, Na(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O, is a new mineral of the tourmaline supergroup. The holotype specimen originates from the locality of Osarara (Narok district, Kenya) and occurs in quartz-muscovite schist. Crystals of oxy-dravite are dark red, partially translucent with a vitreous luster, a pink streak, and conchoidal fracture. It has a Mohs hardness of approximately 7, and a calculated density of 3.073 g/cm3. In plane-polarized light, oxy-dravite is pleochroic (O = orange and E = pink) and uniaxial negative: ω = 1.650(5), ε = 1.620(5). Oxy-dravite is rhombohedral, space group R3m, with the unit-cell parameters a = 15.9273(2) and c = 7.2001(1) Å, V = 1581.81(4) Å3, Z = 3. Chemical characterization based on electron microprobe analysis, single-crystal structure refinement, Mössbauer, and optical spectroscopy, resulted in the empirical structural formula:
X(Na0.83□0.15K0.02)∑1.00Y(Al1.34Fe3+0.58Mg1.03Fe2+0.03Ti0.02)∑3.00Z(Al4.95Mg1.03Fe3+0.02)∑6.00T(Si5.98Al0.02O18)∑6.00B(BO3)3V(OH)3W(O0.76OH0.24)∑1.00.
While the end-member formula of oxy-dravite may be formalized as NaY(Al3)Z(Al4Mg2) Si6O18(BO3)3(OH)3O, the most representative structural formula is NaY(Al2Mg)Z(Al5Mg) Si6O18(BO3)3(OH)3O. The difference between these two formulas is solely in Al-Mg order-disorder, i.e., there is no difference in chemical composition. Although the Mg-Al disorder over the Y and Z sites is controlled by the short-range bond-valence requirements of O2- at the O1 (≡W) site, the amount of Mg at the Z site is a function of the degree of cation size mismatch at Z.
The crystal structure of oxy-dravite was refined to statistical index R1 of 1.17% using 1586 equivalent reflections collected with MoKα X-radiation. Oxy-dravite is chemically related to dravite (and fluor-dravite), NaMg3Al6Si6O18(BO3)3(OH)3(OH,F), by the heterovalent substitution Al3+ + O2- → Mg2+ + (OH,F)1-.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Editorial. Why you should publish your best papers in American Mineralogist: An International Journal of Earth and Planetary Materials
- Highlights and Breakthroughs. New constraints on the size of chondrite parent bodies
- Actinides in Geology, Energy, and the Environment. Further investigation of the initial fission-track length and geometry factor in apatite fission-track thermochronology
- Versatile monazite: Resolving geological records and solving challenges in materials science. Carboniferous inherited grain and age zoning of monazite and xenotime from leucogranites in far-eastern Nepal: Constraints from electron probe microanalysis
- Versatile monazite: Resolving geological records and solving challenges in materials science. Diffusion of helium in natural monazite, and preliminary results on He diffusion in synthetic light rare earth phosphates
- Crystal structure of the high-pressure phase of calcium hydroxide, portlandite: In situ powder and single-crystal X-ray diffraction study
- Experimental development of patch perthite from synthetic cryptoperthite: Microstructural evolution and chemical re-equilibration
- Oxy-dravite, Na(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O, a new mineral species of the tourmaline supergroup
- Behavior of gold in a magma at sulfide-sulfate transition: Revisited
- A disordered nanoparticle model for 6-line ferrihydrite
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- Iron sulfide stoichiometry as a monitor of sulfur fugacity in gas-mixing experiments
- Relaxation effects and re-entrant spin glass behavior at low temperatures in natural strunzite, ferristrunzite, and ferrostrunzite
- Enthalpies of formation of Fe-Ni monosulfide solid solutions
- Influence of temperature and Cl on the hydrothermal replacement of calcite by apatite and the development of porous microstructures
- Ordering state in orthopyroxene as determined by precession electron diffraction
- Interlayer water molecules in organocation-exchanged vermiculite and montmorillonite: A case study of tetramethylammonium
- Spectroscopic and X-ray diffraction investigation of the behavior of hanksite and tychite at high pressures, and a model for the compressibility of sulfate minerals
- Low-temperature magnetism of alabandite: Crucial role of surface oxidation
- Crystallographic and spectroscopic characterization of Fe-bearing chromo-aluminopovondraite and its relations with oxy-chromium-dravite and oxy-dravite
- Experimental determination of siderite stability at high pressure
- Relationships among channel topology and atomic displacements in the structures of Pb5(BO4)3Cl with B = P (pyromorphite), V (vanadinite), and As (mimetite)
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- A comparison of the Ca3(PO4)2 and CaSiO3 systems, with a new structure refinement of tuite synthesized at 15 GPa and 1300 °C
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