Home Physical Sciences An automated system for phase identification and quantitative composition determination using the electron microprobe: Theory and applications
Article
Licensed
Unlicensed Requires Authentication

An automated system for phase identification and quantitative composition determination using the electron microprobe: Theory and applications

  • Kurt Steffen EMAIL logo
Published/Copyright: March 28, 2015
Become an author with De Gruyter Brill

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.

Received: 2004-1-21
Accepted: 2004-5-9
Published Online: 2015-3-28
Published in Print: 2004-10-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. The origin of the color of pearls in iridescence from nano-composite structures of the nacre
  2. “Invisible„ gold revealed: Direct imaging of gold nanoparticles in a Carlin-type deposit
  3. Behavior of cation vacancy in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites
  4. Displacement and strain fields around a [100] dislocation in olivine measured to sub-angstrom accuracy
  5. Kiglapait mineralogy IV: The augite series
  6. Metasomatic formation of kosmochlor-bearing diopside in peridotite xenoliths from North Island, New Zealand
  7. Determination of standard thermodynamic properties of sulfides in the Ag-Au-S system by means of a solid-state galvanic cell
  8. Hydroxyl ordering in igneous apatite
  9. Accommodation of the carbonate ion in apatite: An FTIR and X-ray structure study of crystals synthesized at 2–4 GPa
  10. Mg/Si ratios of aqueous fluids coexisting with forsterite and enstatite based on the phase relations in the Mg2SiO4-SiO2-H2O system
  11. The activity of silica, water, and the equilibration of intermediate and silicic magmas
  12. The CO2–H2O system: IV. Empirical, isothermal equations for representing vapor-liquid equilibria at 110–350 °C, P ≤ 150 MPa
  13. Repercussions of size heterogeneity on the measurement of specific surface areas of colloidal minerals: Combination of macroscopic and microscopic analyses
  14. The crystal-structure of synthetic NaNa2Mg5Si8O21(OH)3, a triclinic C1̄ amphibole with a triple-cell and excess hydrogen
  15. High-pressure phase transitions in Ca0.2Sr0.8Al2Si2O8feldspar
  16. Phase transition of Ca-perovskite and stability of Al-bearing Mg-perovskite in the lower mantle
  17. Mineralogy and petrology of a mullite-bearing pseudotachylyte: Constraints on the temperature of coseismic frictional fusion
  18. New developments in two-feldspar thermometry
  19. Ordered distribution of Au and Ag in the crystal structure of muthmannite, AuAgTe2, a rare telluride from Sacarîmb, western Romania
  20. Polytypism of cookeite in low-grade metapelites of the Cameros Basin, Spain: Lack of correlation of well-ordered polytypes with pressure
  21. Evolution of mineral compositions during eclogitization of subducting basaltic crust
  22. Mass balance during retrogression of eclogite-facies minerals in the Rongcheng eclogite, eastern Sulu ultrahigh-pressure terrane, China
  23. 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
  24. The chemistry and crystal structure of okanoganite-(Y) and comparison with vicanite-(Ce)
  25. An automated system for phase identification and quantitative composition determination using the electron microprobe: Theory and applications
  26. Piston-cylinder calibration at 400 to 500 MPa: A comparison of using water solubility in albite melt and NaCl melting
  27. Letter. Comparative planetary mineralogy: V/(Cr + Al) systematics in chromite as an indicator of relative oxygen fugacity
  28. Letter. Porous titanosilicate nanorods in the structure of yuksporite, (Sr,Ba)2K4(Ca,Na)14(⃞,Mn,Fe) {(Ti,Nb)4(O,OH)4[Si6O17]2[Si2O7]3}(H2O,OH)n, resolved using synchrotron radiation
Downloaded on 24.2.2026 from https://www.degruyterbrill.com/document/doi/10.2138/am-2004-1025/html
Scroll to top button