Abstract
Due to the similar ionic radius of K+ and NH4+, K-silicates can incorporate a significant amount of NH4. As tourmaline is able to accommodate K in its crystal structure at high and ultrahigh pressure, we test if this also holds true for NH4.
Piston-cylinder experiments in the system (NH4)2O-MgO-SiO2-Al2O3-B2O3-H2O at 4.0 GPa, 700 °C, with B2O3 and NH4OH in excess produce an assemblage of tourmaline, phengite, and coesite. The tourmaline crystals are up to 10 × 40 μm in size. EMP analyses indicate that the tourmalines contain 0.22 (±0.03) wt% (NH4)2O and are solid solutions mainly along the magnesio-foitite and “NH4-dravite” join with the average structural formula X[(NH4)0.08(1)o0.92(1)]Y[Mg2.28(8)Al0.72(8)]Z[Al5.93(6)Si0.07(6)]T[Si6.00(5)O18](BO3)3(OH)4.
NH4 incorporation is confirmed by characteristic <N-H> stretching and bending modes in the IR-spectra of single crystals on synthetic tourmaline. Further evidence is the increased unit-cell parameters of the tourmaline [a = 15.9214(9) Å, c = 7.1423(5) Å, V = 1567.9(2) Å3] relative to pure magnesio-foitite.
Incorporation of NH4 in natural tourmaline was tested in a tourmaline-bearing mica schists from a high-P/low-T (>1.2 GPa/550 °C) metasedimentary unit of the Erzgebirge, Germany, rich in NH4. The NH4-concentrations in the three main NH4-bearing phases are: biotite (~1400 ppm) > phengite (~700 ppm) > tourmaline (~500 ppm). This indicates that tourmaline can act as important carrier of nitrogen between the crust and the deep Earth, which has important implications for a better understanding of the large-scale light element cycle.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- The American Mineralogist at 100 years, and a mineralogy renaissance
- At the blurry edge of mineralogy
- Mineral evolution and Earth history
- Franciscan geologic history constrained by tectonic/olistostromal high-grade metamafic blocks in the iconic California Mesozoic-Cenozoic accretionary complex
- The rapid expansion of environmental mineralogy in unconventional ways: Beyond the accepted definition of a mineral, the latest technology, and using nature as our guide
- Microelectronic junctions in arsenian pyrite due to impurity and mixed sulfide heterogeneity
- The structure of water-saturated carbonate melts
- In-situ measurements of fluorine and chlorine speciation and partitioning between melts and aqueous fluids in the Na2O-Al2O3-SiO2-H2O system
- High-pressure high-temperature transitions in MgCr2O4 and crystal structures of new Mg2Cr2O5 and post-spinel MgCr2O4 phases with implications for ultrahigh-pressure chromitites in ophiolites
- Mid-infrared emission spectroscopy and visible/near-infrared reflectance spectroscopy of Fe-sulfate minerals
- Megacrystic zircon with planar fractures in miaskite-type nepheline pegmatites formed at high pressures in the lower crust (Ivrea Zone, southern Alps, Switzerland)
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- Applications of Hirshfeld surfaces to mineralogy: An example of alumohydrocalcite, and the classification of the dundasite group minerals
- Optical absorption anisotropy of high-density, wide-gap, high-hardness SiO2 polymorphs seifertite, stishovite, and coesite
- The system Na2CO3-FeCO3 at 6 GPa and its relation to the system Na2CO3-FeCO3-MgCO3
- Chlorine-hydroxyl diffusion in pargasitic amphibole
- The use of cation-cation and anion-anion bonds to augment the bond-valence model
- AIM analysis and the form of the bond-valence equation
- Atomistic simulation on mixing thermodynamics of calcite-smithsonite solid solutions
- Combined geochemistry and geochronology constrains coupled subduction of oceanic and continental crust in the Huwan shear zone, central China
- Near-infrared investigation of folding sepiolite
- First-principles study of sulfur isotope fractionation in pyrite-type disulfides
- Tetrataenite in terrestrial rock
- Thermo-compression of pyrope-grossular garnet solid solutions: Non-linear compositional dependence
- Phase relationships in the system K2CO3-CaCO3 at 6 GPa and 900–1450 °C
- Trace-element partitioning between plagioclase, alkali feldspar, Ti-magnetite, biotite, apatite, and evolved potassic liquids from Campi Flegrei (Southern Italy)
- Synthetic and natural ammonium-bearing tourmaline
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