مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

969
Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

Information Journal Paper

Title

GEOCHEMICAL BEHAVIOR OF RARE EARTH ELEMENTS IN GARNETS OF KHUT SKARN USING LASER ABLATION ICP-MS DATA, W YAZD, IRAN

Pages

  263-276

Abstract

 The GARNETs from the KHUTSkarn in the west of Yazd have been formed as a result of hydrothermal activity ofOligo-Miocene calc-alkaline plutons. The chemical composition of GARNETs in the KHUTskarn are divided into two solid solution of grossularitic-andraditic and almost pure andradite different types. The Fe-rich GARNETs are isotropic (Adr>96), whereasgrossularitic-andraditic GARNETs are anisotropic and show compositional zoning and sectorial twinning (Ad74.3Gr24.8-Ad32.1Gr66.6). The compositional zoning of anisotropic GARNETs may result from hydrothermal overgrowths on contact metamorphic minerals, variations in P, T, XCO2, concentrations of Fe3+ and Al, or kinetic factors. The Laser Ablation ICP-MS results show isotropic GARNETs exhibit LREE-enriched and HREE-depleted patterns, with a positive Eu anomaly. These GARNETs grow rapidly under relatively high W/R ratios from the magmatic-derived fluids during infiltration METASOMATISM process, whereas anisotropic GARNETs have much lower enrichment in LREE and show a weak negative Eu anomaly. These GARNETs formed by prolonged interaction of pore fluids with the host rocks during the diffusive METASOMATISM process.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    ZAHEDI, A., BOOMERI, M., & MACKIZADEH, M.A.. (2015). GEOCHEMICAL BEHAVIOR OF RARE EARTH ELEMENTS IN GARNETS OF KHUT SKARN USING LASER ABLATION ICP-MS DATA, W YAZD, IRAN. GEOSCIENCES, 24(94 (PETROLOGY & MINERALOGY)), 263-276. SID. https://sid.ir/paper/31341/en

    Vancouver: Copy

    ZAHEDI A., BOOMERI M., MACKIZADEH M.A.. GEOCHEMICAL BEHAVIOR OF RARE EARTH ELEMENTS IN GARNETS OF KHUT SKARN USING LASER ABLATION ICP-MS DATA, W YAZD, IRAN. GEOSCIENCES[Internet]. 2015;24(94 (PETROLOGY & MINERALOGY)):263-276. Available from: https://sid.ir/paper/31341/en

    IEEE: Copy

    A. ZAHEDI, M. BOOMERI, and M.A. MACKIZADEH, “GEOCHEMICAL BEHAVIOR OF RARE EARTH ELEMENTS IN GARNETS OF KHUT SKARN USING LASER ABLATION ICP-MS DATA, W YAZD, IRAN,” GEOSCIENCES, vol. 24, no. 94 (PETROLOGY & MINERALOGY), pp. 263–276, 2015, [Online]. Available: https://sid.ir/paper/31341/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top