Abstract
Typical liquidus temperatures can be over 1000°C greater than the glass transition temperatures for high-pressure aluminosilicate melts so the effect of temperature must be determined if glass data is to be used to approximate the structural speciation present in geologic melts. This study has investigated the effect of fictive temperature (Tf, taken as the temperature where the melt structure is the same as that of the glass) on the percentage of [5]Al and [6]Al species in two high-pressure (10 GPa) Na-aluminosilicate glasses (Na3AlSi7O17 and NaAlSi3O8) where one glass of each composition was quenched from the high-pressure melt while the other was annealed near the glass transition temperature. The 27Al MAS NMR spectra of the Na3AlSi7O17 samples show that the higher Tf (quenched) glass contains more high-coordinated Al than the lower Tf (annealed, 475°C) glass. However, the 27Al spectra of the NaAlSi3O8 samples show the opposite temperature dependency, which in addition to the lack of NBO in this glass, may suggest differing mechanisms for the generation of high-coordinated Al
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Crystal-size and shape distributions of magnetite from uncultured magnetotactic bacteria as a potential biomarker
- Tourmaline-bearing rocks in the Singhbhum shear zone, eastern India: Evidence of boron infiltration during regional metamorphism
- High-resolution transmission electron microscopy (HRTEM) study of the 4a and 6a superstructure of bornite Cu5FeS4
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- Direct observation of spinodal decomposition in the magnetite-hercynite system by susceptibility measurements and transmission electron microscopy
- Thermodynamics of uranyl minerals: Enthalpies of formation of rutherfordine, UO2CO3, andersonite, Na2CaUO2(CO3)3(H2O)5, and grimselite, K3NaUO2(CO3)3H2O
- Mixing and ordering behavior in manganocolumbite-ferrocolumbite solid solution: A single-crystal X-ray diffraction study
- Structure change of MgSiO3, MgGeO3, and MgTiO3 ilmenites under compression
- Dehydration processes in the meta-autunite group minerals meta-autunite, metasaléeite, and metatorbernite
- Investigation of the martensitic-like transformation from Mg2GeO4 olivine to its spinel structure polymorph
- A high-temperature diffraction study of the solid solution CaTiOSiO4-CaTiOGeO4
- The vibrational spectrum of synthetic hydrogrossular (katoite) Ca3Al2(O4H4)3: A low-temperature IR and Raman spectroscopic study
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- Synthesis and crystal-chemistry of alkali amphiboles in the system Na2O-MgO-FeO-Fe2O3- SiO2-H2O as a function of fO2
- Compositional zoning in sphalerite crystals
- Structure and the extent of disorder in quaternary (Ca-Mg and Ca-Na) aluminosilicate glasses and melts
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- Early diagenetic origin of Al phosphate-sulfate minerals (woodhouseite and crandallite series) in terrestrial sandstones, Nova Scotia, Canada
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