Abstract
The single-crystal X-ray technique was used to calibrate a new intracrystalline geothermometer based on equilibrium Mg-Fe* fractionation (Fe* = Fe2+ + Mn2+) between M1 and M2 sites of natural P21/c pigeonite. Suitable crystals free of exsolution textures and sharp diffraction maxima were selected by careful TEM and XRD investigations from a large number of samples. Two single crystals, PCA82506-3 (Wo6En76Fs18) from the Pecora Escarpment 82506 Antarctic ureilite, and BTS308- 2 (Wo10En47Fs43) from the BTS308 Paranà rhyodacite, were annealed at temperatures ranging from 600 to 1000 °C. The TEM investigation, carried out on fragments of selected single crystals both before and after thermal treatment, shows heating-induced texture modifications preliminary to spinodal decomposition in both crystals and a size increase in antiphase domains in BTS308-2. The two geothermometric equations calculated by linear regression of ln KD* vs. 1/T are:
ln KD* = -3291(± 269)/T(K) + 0.971(±0.253); (r2 = 0.974)
ln KD* = -2816(± 83)/T(K) + 0.542(±0.083); (r2 = 0.995)
respectively for PCA82506-3 (XFe* = 0.20) and BTS308-2 (XFe* = 0.49) [XFe* = Fe*/(Fe* + Mg)]. These results imply negligible compositional effects on Mg-Fe* site partitioning within the range of compositions encompassed by the samples. Comparison of the intracrystalline fractionation data of pigeonites with those of Pbca orthopyroxenes shows a similar degree of ordering for both at a given temperature. This result suggests only a small effect of Ca on Fe*-Mg ordering in pyroxene with Ca content up to Wo10-.
© 2015 by Walter de Gruyter Berlin/Boston
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- Cerium anomaly and Th/U fractionation in the 1.85 Ga Flin Flon Paleosol: Clues from REE- and U-rich accessory minerals and implications for paleoatmospheric reconstruction
- Os solubility in silicate melts: New efforts and results
- Enstatite-forsterite-water equilibria at elevated temperatures and pressures
- The OH-F substitution in synthetic pargasite at 1.5 kbar, 850 °C
- Uptake of aqueous Pb by Cl-, F–, and OH– apatites: Mineralogic evidence for nucleation mechanisms
- Temperature dependence of the hyperfine parameters of synthetic P21/c Mg-Fe clinopyroxenes along the MgSiO3-FeSiO3 join
- Single-crystal thermometric calibration of Fe-Mg order-disorder in pigeonites
- TEM observations on the P1̄ -I1̄ phase transition in feldspars along the join CaAl2Si2O8-SrAl2Si2O8
- Phase transitions induced by solid solution in stuffed derivatives of quartz: A powder synchrotron XRD study of the LiAlSiO4-SiO2 join
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- The transformation of andalusite to mullite and silica: Part II. Transformation mechanisms in [100]A and [010]A directions
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- The equation of state of lawsonite to 7 GPa and 873 K, and calculation of its high pressure stability
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- 113Cd double-resonance NMR as a probe of clay mineral cation exchange sites
- Solid state NMR study of oxygen site exchange and Al-O-Al site concentration in analcime
- Isomorphous substitution effect on the vibration frequencies of hydroxyl groups in molecular cluster models of the clay octahedral sheet
- Molecular modeling of the structure and dynamics of the interlayer and surface species of mixed-metal layered hydroxides: Chloride and water in hydrocalumite (Friedel’s salt)
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Articles in the same Issue
- Application of new experimental and garnet Margules data to the garnet-biotite geothermometer
- Volumes of mixing in aluminosilicate garnets: Solid solution and strain behavior
- Cerium anomaly and Th/U fractionation in the 1.85 Ga Flin Flon Paleosol: Clues from REE- and U-rich accessory minerals and implications for paleoatmospheric reconstruction
- Os solubility in silicate melts: New efforts and results
- Enstatite-forsterite-water equilibria at elevated temperatures and pressures
- The OH-F substitution in synthetic pargasite at 1.5 kbar, 850 °C
- Uptake of aqueous Pb by Cl-, F–, and OH– apatites: Mineralogic evidence for nucleation mechanisms
- Temperature dependence of the hyperfine parameters of synthetic P21/c Mg-Fe clinopyroxenes along the MgSiO3-FeSiO3 join
- Single-crystal thermometric calibration of Fe-Mg order-disorder in pigeonites
- TEM observations on the P1̄ -I1̄ phase transition in feldspars along the join CaAl2Si2O8-SrAl2Si2O8
- Phase transitions induced by solid solution in stuffed derivatives of quartz: A powder synchrotron XRD study of the LiAlSiO4-SiO2 join
- The transformation of andalusite to mullite and silica: Part I. Transformation mechanism in [001]A direction
- The transformation of andalusite to mullite and silica: Part II. Transformation mechanisms in [100]A and [010]A directions
- Structure and twinning of tetragonal Ca3Mn2Ge3O12 garnet
- The equation of state of lawsonite to 7 GPa and 873 K, and calculation of its high pressure stability
- Boron K-edge XANES of borate and borosilicate minerals
- 113Cd double-resonance NMR as a probe of clay mineral cation exchange sites
- Solid state NMR study of oxygen site exchange and Al-O-Al site concentration in analcime
- Isomorphous substitution effect on the vibration frequencies of hydroxyl groups in molecular cluster models of the clay octahedral sheet
- Molecular modeling of the structure and dynamics of the interlayer and surface species of mixed-metal layered hydroxides: Chloride and water in hydrocalumite (Friedel’s salt)
- VIII(Mg,Fe)0.85VI(Mg,Fe)4IV(Fe,Ge)3O12: A new tetragonal phase and its comparison with garnet
- Rietveld analysis of dicalcium aluminate (Ca2Al2O5) – A new high pressure phase with the Brownmillerite-type structure
- Suredaite, PbSnS3, a new mineral species, from the Pirquitas Ag-Sn deposit, NW-Argentina: mineralogy and crystal structure
- Kozoite-(Nd), Nd(CO3)(OH), a new mineral in an alkali olivine basalt from Hizen-cho, Saga Prefecture, Japan
- Florenskyite, FeTiP, a new phosphide from the Kaidun meteorite
- Letters. Computer simulation of high-temperature, forsterite-melt partitioning