Abstract
Previously developed methods of phase classification using the electron microprobe have been based on setting threshold values or relative ranks for wt% oxide values. These methods perform poorly for minerals that have a significant solid solution, and provide no mechanism for checking the accuracy of the analysis or the accuracy of the classification. Because of these limitations, previous algorithms for phase classification cannot be completely automated to yield high-quality phase classifications for a broad range of assemblages. A new algorithm for phase classification using a transformation from wt% oxide to cation and finally to additive/exchange components is introduced. This algorithm can be completely automated, evaluates the accuracy of the mineral analysis and phase classification, and provides quantitative information about the composition of the phase. The algorithm works by exploiting the least-squares nature of the transformation from wt% oxide to additive/exchange components. This transformation determines the stoichiometric model-mineral composition nearest to the actual mineral composition (in a weighted least-squares sense). The difference between the stoichiometric model composition and the actual composition is determined for all possible phases. The stoichiometric model that has the smallest difference between the model and actual composition and has permissible values for the exchange components identiÞ es the phase. If no stoichiometric mineral model fulfills these requirements (non-permissible exchange components or large difference between actual and model compositions), then the analysis is either of poor quality or there is no stoichiometric model available for the phase being analyzed.
The ability of this algorithm to provide robust, automated phase classification and compositional analysis allows the electron microprobe to be used for modal analysis, as well as analysis of compositional variation with a phase and many other applications. The MATLAB package APHID (Additive/ exchange PHase IDentification) implements this algorithm.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- The origin of the color of pearls in iridescence from nano-composite structures of the nacre
- “Invisible„ gold revealed: Direct imaging of gold nanoparticles in a Carlin-type deposit
- Behavior of cation vacancy in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites
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- Metasomatic formation of kosmochlor-bearing diopside in peridotite xenoliths from North Island, New Zealand
- Determination of standard thermodynamic properties of sulfides in the Ag-Au-S system by means of a solid-state galvanic cell
- Hydroxyl ordering in igneous apatite
- Accommodation of the carbonate ion in apatite: An FTIR and X-ray structure study of crystals synthesized at 2–4 GPa
- Mg/Si ratios of aqueous fluids coexisting with forsterite and enstatite based on the phase relations in the Mg2SiO4-SiO2-H2O system
- The activity of silica, water, and the equilibration of intermediate and silicic magmas
- The CO2–H2O system: IV. Empirical, isothermal equations for representing vapor-liquid equilibria at 110–350 °C, P ≤ 150 MPa
- Repercussions of size heterogeneity on the measurement of specific surface areas of colloidal minerals: Combination of macroscopic and microscopic analyses
- The crystal-structure of synthetic NaNa2Mg5Si8O21(OH)3, a triclinic C1̄ amphibole with a triple-cell and excess hydrogen
- High-pressure phase transitions in Ca0.2Sr0.8Al2Si2O8feldspar
- Phase transition of Ca-perovskite and stability of Al-bearing Mg-perovskite in the lower mantle
- Mineralogy and petrology of a mullite-bearing pseudotachylyte: Constraints on the temperature of coseismic frictional fusion
- New developments in two-feldspar thermometry
- Ordered distribution of Au and Ag in the crystal structure of muthmannite, AuAgTe2, a rare telluride from Sacarîmb, western Romania
- Polytypism of cookeite in low-grade metapelites of the Cameros Basin, Spain: Lack of correlation of well-ordered polytypes with pressure
- Evolution of mineral compositions during eclogitization of subducting basaltic crust
- Mass balance during retrogression of eclogite-facies minerals in the Rongcheng eclogite, eastern Sulu ultrahigh-pressure terrane, China
- Synthesis of REE and Y phosphates by Pb-free flux methods and their utilization as standards for electron microprobe analysis and in design of monazite chemical U-Th-Pb dating protocol
- The chemistry and crystal structure of okanoganite-(Y) and comparison with vicanite-(Ce)
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